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Artículos de revistas sobre el tema "Geology of Germany"

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Publicado: 26 de julio de 2024
Última modificación: 27 de julio de 2024

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1

Gross, W. y H. P. Schultze. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin. Teil 6: Geschichte des Geologisch-Paläontologischen Instituts und Museums der Universität Berlin 1910–2004". Fossil Record 7, n.º 1 (1 de enero de 2004): 5–43. http://dx.doi.org/10.5194/fr-7-5-2004.

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Die Entwicklung des Geologisch-Paläontologischen Instituts und Museums der Universität Berlin von einer Institution, die Geologie zusammen mit Paläontologie als eine Einheit vertrat, über eine Institution, die eine geotektonische Ausrichtung hatte, zu einer auf Paläontologie konzentrierten Institution wird nachvollzogen. Die beiden Institutsdirektoren am Anfang des 20sten Jahrhunderts waren Vertreter der allumfassenden Geologie des 19ten Jahrhunderts, während die beiden folgenden Direktoren eine Geologie ohne Paläontologie vertraten. Das führte zu einer Trennung der beiden Richtungen, und nach der III. Hochschulreform der DDR 1968 verblieb allein die sammlungsbezogene Paläontologie am Museum. Nach der Wiedervereinigung wurde ein Institut für Paläontologie mit biologischer Ausrichtung mit zwei Professuren, einer für Paläozoologie und einer für Paläobotanik, eingerichtet. <br><br> The development of the Geologisch-Paläontologisches Institut und Museum of the Museum für Naturkunde at the Humboldt University (formerly Friedrich-Wilhelm-Universität) in Berlin from a geology-paleontology institution to a pure paleontology institution is described. The first two directors of the department in the beginning of the 20th century, Prof, von Branca and Prof. Pompeckj, represented a 19th century concept of a geology, which included paleontology, even vertebrate paleontology as the crown jewel of geology. They fought sometimes vigorously against a separation of paleontology from geology. The next two directors. Prof. Stille and Prof, von Bubnoff, were the leading geologists in Germany; to be a student of Stille was a special trade mark in geology of Germany. They represented a geology centered on tectonics. The separation of paleontology as separate section was prepared. The destructions of the Second World War, the following restaurations and the division of Germany into two States influenced strongly their directorships. The education of geologists at the Museum für Naturkunde ended with the III. University Reform of the German Democratic Republik in 1968. Paleontology was represented by the international renown vertebrate paleontologist, Prof. Dr. W. Gross, up to 1961. Since 1969, paleobotany was strengthened by the inclusion of the paleobotany unit of the Akademie der Wissenschaften into the museum. After reunification of Germany n 1990, the department was rebuild as a Institut für Palaontologie with close connection to biology, a unique situation in Germany. Two professorships, one for paleozoology, Prof. Schultze. and one for paleobotany, Prof. Mai, were established. The number of curators increased to ten from one under the first director of the 20th century. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20040070103" target="_blank">10.1002/mmng.20040070103</a>
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2

Kölbl-Ebert, Martina. "Geology in Germany 1933–1945: People, politics and organization". Earth Sciences History 36, n.º 1 (1 de enero de 2017): 63–100. http://dx.doi.org/10.17704/1944-6178-36.1.63.

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This paper explores geology in Germany during the Third Reich, 1933–1945. It deals with the effect of the political regime on the daily life in institutes and universities, with victims, perpetrators and bystanders, with geologists supporting the regime with their expertise in administration, economy and military, with ideological influences on geology as such and most of all with German geologists of that time and the broad spectrum of attitudes they cultivated.
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3

Quade, Horst y Ernst-Rüdiger Look. "Fascination Geology – The most important geosites of Germany". Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 66 (28 de mayo de 2010): 81–82. http://dx.doi.org/10.1127/sdgg/66/2010/81.

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4

Martin, Tina y Katrin Schwalenberg. "Full Spectrum". Leading Edge 39, n.º 2 (febrero de 2020): 145–46. http://dx.doi.org/10.1190/tle39020145.1.

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The German Geophysical Society (Deutsche Geophysikalische Gesellschaft, DGG) was founded in 1922 in Leipzig, Germany, on the initiative of the famous German seismologist Emil Wiechert (1861–1928), known for his fundamental work to record earthquake waves to study the earth's interior. Facing the German historical background of the early 20th century, the 24 founding members wanted to lead German geophysicists out of isolation and toward outreaching activities. DGG always understood and defined geophysics as a discipline beyond political borders, religious belief, or race, and promoted the scientific exchange between geophysicists in the Federal Republic of Germany, the former German Democratic Republic, and internationally.
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5

Kockel, F. "Rifting processes in NW-Germany and the German North Sea Sector". Netherlands Journal of Geosciences - Geologie en Mijnbouw 81, n.º 2 (agosto de 2002): 149–58. http://dx.doi.org/10.1017/s0016774600022381.

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AbstractSince the beginning of the development of the North German Basin in Stephanien to Early Rotliegend times, rifting played a major role. Nearly all structures in NW-Germany and the German North Sea - (more than 800) - salt diapirs, grabens, inverted grabens and inversion structures - are genetically related to rifting. Today, the rifting periods are well dated. We find signs of dilatation at all times except from the Late Aptian to the end of the Turonian. To the contrary, the period of the Coniacian and Santonian, lasting only five million years was a time of compression, transpression, crustal shortening and inversion. Rifting activities decreased notably after inversion in Late Cretaceous times. Tertiary movements concentrated on a limited number of major, long existing lineaments. Seismically today NW-Germany and the German North Sea sector is one of the quietest regions in Central Europe.
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6

Seifert, Andreas, Hermann Brause y Jochen Rascher. "Geology of the Niederlausitz Lignite district, Germany". International Journal of Coal Geology 23, n.º 1-4 (septiembre de 1993): 263–89. http://dx.doi.org/10.1016/0166-5162(93)90052-c.

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7

Zuhr, Alexandra M., Erik Loebel, Marek Muchow, Donovan Dennis, Luisa von Albedyll, Frigga Kruse, Heidemarie Kassens et al. "Insights into German polar research during POLARSTUNDE". Polarforschung 91 (26 de octubre de 2023): 73–80. http://dx.doi.org/10.5194/polf-91-73-2023.

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Abstract. Polar research is an interdisciplinary and multi-faceted field of research ranging from history to geology and geophysics to social sciences and education. Thus, several different universities and institutions within Germany participate in polar research. The seminar series POLARSTUNDE, organized by the German Society for Polar Research (Deutsche Gesellschaft für Polarforschung) and the German National Committee of the Association of Polar Early Career Scientists (APECS Germany) regularly features different topics of German polar research. Although initially a “pandemic solution”, the seminar series has established itself as a valuable and highly successful part of the German polar research landscape. The seminar series was held in German and was aimed at both scientists and the general public. This article addresses the first season of POLARSTUNDE and provides (1) comprehensive summaries of the talks and (2) insight into the planning and execution from an organizational point of view.
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8

Hadden, R. "The Heringen Collection of the US Geological Survey Library, Reston, Virginia". Earth Sciences History 27, n.º 2 (3 de noviembre de 2008): 242–65. http://dx.doi.org/10.17704/eshi.27.2.y1vq1168q51g1542.

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A special collection of German, Polish, and Russian language books, maps and reports in the US Geological Survey Library has an interesting and unusual history. The so-called ‘Heringen Collection’ came from Nazi Germany. Many of these items were captured from libraries, offices and even private homes as the German Army advanced into neighboring countries. In the last days of the war, these maps, reports, photos and other records were sent from the Military Geology offices in Berlin to the safety of a deep potash mineshaft in Heringen (Werra), in Hessen, Germany. A group of US Army soldiers found these lost records of the Third Reich. When removed from the Heringen mine, those records that dealt with the earth sciences, terrain analysis, military geology and other geological matters were sent to the USGS, and eventually came to reside at the USGS Library. The printed papers and books were mostly incorporated into the main collection, but a portion of the materials have never been cataloged, calendared or indexed. These materials have many current uses, including projects of value to citizens in their nations of origin.
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9

Mohr, Barbara y Annette Vogt. "German Women Paleobotanists From the 1920S to the 1970S—Or Why Did This Story Start So Late?" Earth Sciences History 20, n.º 1 (1 de enero de 2001): 14–43. http://dx.doi.org/10.17704/eshi.20.1.q7643x2308728m56.

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This study documents women paleobotanists and their achievements from the late 1920s to the early 1970s in Germany. More than forty women were involved in paleobotanical research and related fields during this period. After they had finished their degrees, about two thirds of them left the field for private, political, and/or economic reasons. Several of them, however, had a successful career or were even leaders in their field. Compared with other disciplines and neighbouring countries, the unusually late entry of women students into this discipline from the 1930s on is explained by the close affiliation of the discipline with Paleozoic geology and mining in Germany before 1945. It is significant that of the thirteen women who finished a degree in the field before 1945, about two thirds studied Quaternary pollen analysis and vegetation history. Only a minority was involved in pre-Quaternary paleobotany. After World War II, the number of women scientists increased noticeably only when Tertiary palynology/paleobotany became more important sub-disciplines of paleobotany, a pattern which was similar in both parts of the newly divided country. During the period between 1945 and 1955, the number of women students in West Germany was significantly higher than in the East. This is partly explained by the policies of the East German communist party, which put restrictions on women students from a middle-class background. Between 1955 and 1973 the number of women students in East Germany exceeded those in the West. This was due to the East German party policy of activating the female working force, especially in fields which had been traditionally occupied by men, such as geology, mining, and engineering.
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10

Vejbæk, Ole Valdemar. "Tectonic atlas of Northwest Germany and the German North Sea sector". Bulletin of the Geological Society of Denmark 49 (26 de junio de 2002): 91. http://dx.doi.org/10.37570/bgsd-2003-49-16.

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11

CLARY, RENEE M. "THE ROYAL SCHOOL OF MINES: HENRY DE LA BECHE’S CONVERGENCE OF PROFESSIONALIZATION AND PUBLIC ADVOCACY". Earth Sciences History 39, n.º 2 (12 de noviembre de 2020): 291–304. http://dx.doi.org/10.17704/1944-6187-39.2.291.

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ABSTRACT Several European countries instituted mining schools in the late 1700s, including France, Germany, Hungary, and Russia. However, since England’s mining industry was privatized with little government involvement, Great Britain was decades behind with the creation of a school of mines. In 1835, Henry De la Beche (1796–1855) became the first director of the Ordnance Geological Survey, precursor to the British Geological Survey. De la Beche used this position to advance geology’s professionalization, which would include the establishment of an applied geology museum, mining records storehouse, and a school of mines. The Museum of Economic Geology, displaying the country’s mineral resources and geology, was De la Beche’s first success. Founded in 1835, it opened to the public in 1841. The Mining Records Office opened in 1840 as a repository for plans of working and abandoned mines. An early public advocate for workers’ safety, De la Beche lobbied for government inspections of collieries, immediate reporting of mining accidents, and proper plans of mines. The School of Mines was De la Beche’s third accomplishment in geology’s professionalization. As an outgrowth of the museum, it was formally opened in 1851 along with the larger Museum of Practical Geology, the Museum of Economic Geology’s successor. De la Beche’s intent for the School of Mines—instruction as a combination of science and practice—seems modern in its approach. In 1843, funding was allocated for lectures on the practical applications of geology, but these were not implemented until the School of Mines opened in 1851. In his effort to educate everyone—from miner to mine owner—De la Beche transcended social boundaries and supported open, public lectures. As a result, some considered him a class traitor. De la Beche used his position to advocate for advancement of the mining industry to include miner safety and public education. Therefore, while the Royal School of Mines emerged later than many of its European counterparts, it was part of a systematic professionalization of geology, coupled with education and a public advocacy for mining participants.
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12

Cook, Robert B. "Stannite Freiberg, Saxony, Germany". Rocks & Minerals 81, n.º 6 (enero de 2006): 458–61. http://dx.doi.org/10.3200/rmin.81.6.458-461.

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13

Massanek, Andreas y Christina Seifert. "German Minerals in the Krügerhaus, A New Permanent Exhibition in Freiberg, Saxony, Germany". Rocks & Minerals 88, n.º 3 (mayo de 2013): 212–21. http://dx.doi.org/10.1080/00357529.2013.777607.

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14

SACHS, SVEN, MARKUS WILMSEN, JOSCHUA KNÜPPE, JAHN J. HORNUNG y BENJAMIN P. KEAR. "Cenomanian–Turonian marine amniote remains from the Saxonian Cretaceous Basin of Germany". Geological Magazine 154, n.º 2 (22 de enero de 2016): 237–46. http://dx.doi.org/10.1017/s0016756815001004.

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AbstractThe Saxonian Cretaceous Basin constitutes an important source of rare Late Cretaceous marine amniote fossils from Germany. It is also historically famous, having been documented in a series of monographic works published by the distinguished German palaeontologist Hanns Bruno Geinitz in the nineteenth century. The most productive rock units include the upper Cenomanian Dölzschen Formation and upper Turonian Strehlen and Weinböhla limestones (lower Strehlen Formation). A survey of curated specimens recovered from these deposits has now identified isolated teeth of probable polycotylid and elasmosaurid plesiosaurians, as well as several humeri that are referred to protostegid marine turtles. The Saxonian Cretaceous Basin formed a continuous epeiric seaway with the Bohemian Cretaceous Basin during late Cenomanian – Turonian time. A western connection to the North Sea Basin also existed via the North German and Münsterland Cretaceous basins. The Mesozoic marine amniote remains from these regions therefore record a coeval northern European fauna that was probably homogeneous across the northern peri-Tethyan margin during Late Cretaceous time.
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15

El Hourani, Mariam El, Joachim Härtling y Gabriele Broll. "Hydromorphological Assessment as a Tool for River Basin Management: Problems with the German Field Survey Method at the Transition of Two Ecoregions". Hydrology 9, n.º 7 (30 de junio de 2022): 120. http://dx.doi.org/10.3390/hydrology9070120.

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Since the Water Framework Directive (WFD) came into force in 2000, data on the hydromorphological quality have been collected for all rivers in Europe. In Germany, a reference-based classification scheme is used (LAWA 2000) for hydrological assessment. The question arises whether this method can compensate sufficiently for a change of ecoregion. In our study of the Hase River in NW Germany, the frequency of the river classes was compared between two ecoregions (Lower Saxonian Mountains vs. Northwest-German Lowlands). In the lowlands, the evaluation shows a significantly higher proportion of class 5 river sections. This can mainly be attributed to the main parameters, longitudinal section, riverbed structure and bank structure. While the bad results in the longitudinal section and bank structure can be explained by changes in geology and anthropogenic pressures, the evaluation scheme cannot sufficiently compensate for changes in the riverbed structure. This problem is aggravated by the inconsistent implementation of the evaluation scheme in Germany, where the federal states use different approaches with regard to section length. Using 100 m sections throughout the river course can lead to severely underestimating the number of structures. Further improvement and standardization in the evaluation scheme seem to be necessary for the adjustment of the field survey method to different ecoregions in Germany.
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16

Katzung, G., U. Giese, R. Walter y C. Von Winterfeld. "The Rügen Caledonides, northeast Germany". Geological Magazine 130, n.º 5 (septiembre de 1993): 725–30. http://dx.doi.org/10.1017/s0016756800021038.

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AbstractBorehole evidence from the Isle of Rügen, and geophysical data from the adjacent Baltic Sea suggest a Caledonian deformation front that caused NNE-directed thrusting on the East European Platform. It is thought to mark a Caledonian suture zone which was reactivated in syn- to post-Variscan events to form the Rømiø-Møn Fault Zone.
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17

Reiche, Sönke, Lukas Alexander Schröder y Diana Hermann. "The collection, digitisation, interpretation and publication of geological data in the German site selection procedure – status and challenges". Safety of Nuclear Waste Disposal 2 (6 de septiembre de 2023): 141. http://dx.doi.org/10.5194/sand-2-141-2023.

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Abstract. The German site selection procedure for a repository site for high-level nuclear waste is subdivided into three major phases. During the first phase, the subsurface of Germany is evaluated based on existing data, with the aim of defining siting regions for surface-based underground exploration. Although Germany is covered by large amounts of geoscientific data – including ca. 50 000 boreholes deeper than 300 m and more than 340 000 km of reflection seismic lines – the legal obligation to make these data publicly available on a national scale is fairly new and dates back to the Geological Data Act of 2020 (GeolDG: Geologiedatengesetz vom 19. Juni 2020; BGBl. I S. 1387). However, significant amounts of data are available in analogue form only, posing a significant challenge to the timeline of the site selection procedure. As the German nuclear waste management organisation, the Federal Company for Radioactive Waste Disposal (BGE) is in charge of collecting, interpreting and publishing geoscientific data that are relevant to the decisions made within the site selection procedure. In this contribution, we outline the path of data within the first phase of the site selection procedure. We start with an overview of the BGE's current and past activities related to data collection and digitisation, focussing on a major campaign through which more than 16 000 drilling reports are being digitised in cooperation with the State Office for Mining, Energy and Geology in Lower Saxony (LBEG). We then report on the different approaches of data quality control, processing and supply, highlighting challenges related to the federal organisation of geodata storage in Germany. We present selected examples of how data are used for evaluating the subsurface in terms of suitability as a potential repository site. Finally, we give an outlook of how data could be integrated into a web application that is currently being developed as an interactive tool for the public presentation of results and underlying decisions.
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18

Cook, Robert B. "Connoisseur's Choice: Manganite Ilfeld, Harz, Germany". Rocks & Minerals 74, n.º 4 (enero de 1999): 250–52. http://dx.doi.org/10.1080/00357529909602547.

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19

Ziegler, Peter A. "Tectonic atlas of NW Germany". Marine and Petroleum Geology 14, n.º 7-8 (noviembre de 1997): 1013–14. http://dx.doi.org/10.1016/s0264-8172(97)00047-0.

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20

Mohr, B. A. R. y A. Vogt. "Berliner Geowissenschaftlerinnen an der Friedrich-Wilhelms-Universität von 1906 bis 1945, eine Fallstudie". Fossil Record 6, n.º 1 (1 de enero de 2003): 53–69. http://dx.doi.org/10.5194/fr-6-53-2003.

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In dieser Untersuchung werden beispielhaft die Lebenswege und Karrieren von Berliner Geowissenschaftlerinnen im Zeitraum von 1906 bis 1945 nachgezeichnet und analysiert. Ähnlich wie an anderen deutschen bzw. westlichen Universitäten, aber im Gegensatz zu Russland, begann die Tätigkeit von Frauen in den Geowissenschaften spät, und das Fach wurde auch relativ selten gewählt, hauptsächlich wegen der zu geringen Berufschancen. Aber die besondere Situation in Berlin mit mehreren sich ergänzenden Institutionen und dem daraus resultierenden breiten Spektrum an geowissenschaftlichen Disziplinen, sowie ausgezeichneten Professoren, ließ dennoch Raum für eine Ausbildung in diesem Bereich und erlaubte, wenn auch in bescheidenem Maße, eine gewisse Karrieremöglichkeit. <br><br> Während der hier untersuchten 40 Jahre haben weniger als 20 Frauen in den Geowissenschaften und benachbarten Gebieten promoviert. Mehrere dieser Frauen blieben in dem von ihnen gewählten Fach weiterhin aktiv und wurden erfolgreich. Zwei Frauen gelang eine akademische Karriere — eine als Universitätsprofessorin, die auch Schülerinnen hatte. Andere arbeiteten an staatlichen Institutionen, wie z. B. dem Geologischen Landesamt. Wenige Frauen blieben nach ihrer Verheiratung beruflich aktiv, wenn auch nicht offiziell angestellt, sondern als Ehefrauen. Andere arbeiteten als "Ersatz" für die im Kriege stehenden Männer. Einige waren aus persönlichen und politischen Gründen, insbesondere während der NS-Zeit, gezwungen, die Geowissenschaften zu verlassen, konnten aber teilweise auf anderen Gebieten erfolgreich arbeiten. <br><br> This paper documents the lives and careers of women geoscientists at the Berlin Friedrich-Wilhelms-University from 1906 through 1945. Traditionally, in Germany, women had difficulties to be accepted in geosciences (except for geography/geology teachers), because of strong links between geology and mining, a field dominated clearly by men. In western European countries, as well as in the U.S.A. and Australia, the situation was similar in that women started late and in small numbers to study geology. This was, however, in contrast to Russia and later the Soviet Union where women were relatively early accepted even as university teachers. <br><br> The data for this paper were gathered from Berlin University institutions, such as the historical archive and the library of the Palaeontological Institute, and in addition personal contacts were used. Women who had studied either geography, geology/palaeontology, geophysics, mineralogy or botany/palaeobotany are subject of this study. Only those are considered who had strong affiliations to geosciences proper, in all 17 women. <br><br> During the first half of the 20th century the Berlin Friedrich-Wilhelms-University, founded in 1810, was one of the most important institutions concerning higher education in Germany, especially for women. The official opening of this university for women students was in 1908, somewhat later than at other German universities. Once admitted, however, the number of dissertations completed by women was relatively high, and, 30% of all habilitations (advanced degree which allows teaching at universities) in Germany and 50% of all habilitations in the natural sciences were accomplished at Berlin between 1918/19 to 1932. <br><br> The geosciences were, together with medicine, chemistry, physics, botany and zoology, very strong scientifical and in teaching. Geoscientists of international reputation worked at large institutions, affiliated or being part of the University, such as the Prussian (later German) Geological Survey, the Institute of Geology and Palaeontology at the Museum of Natural History or the Institute and Museum of Oceanography, and were the advisers and reviewers of women Diploma and PhD students. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20030060103" target="_blank">10.1002/mmng.20030060103</a>
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21

El-Kelani, R., G. Jentzsch y U. Schreiber. "Gravity anomalies and subsurface geology in the Westerwald volcanic area, Germany". Geologische Rundschau 87, n.º 3 (14 de diciembre de 1998): 381–93. http://dx.doi.org/10.1007/s005310050217.

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22

Van der Wateren, Frederik M. "Structural geology and sedimentology of the Heiligenhafen till section, Northern Germany". Quaternary Science Reviews 18, n.º 14 (diciembre de 1999): 1625–39. http://dx.doi.org/10.1016/s0277-3791(98)00120-6.

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23

Schindler, Thomas y Michael Wuttke. "Geology and limnology of the Enspel Formation (Chattian, Oligocene; Westerwald, Germany)". Palaeobiodiversity and Palaeoenvironments 90, n.º 1 (18 de noviembre de 2009): 21–27. http://dx.doi.org/10.1007/s12549-009-0014-4.

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24

Guntau, Martin. "The rise of geology as a science in Germany around 1800". Geological Society, London, Special Publications 317, n.º 1 (2009): 163–77. http://dx.doi.org/10.1144/sp317.9.

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25

Schäfer, Andreas, Torsten Utescher y Thomas Mörs. "Stratigraphy of the Cenozoic Lower Rhine Basin, northwestern Germany". Newsletters on Stratigraphy 40, n.º 1-2 (1 de junio de 2004): 73–110. http://dx.doi.org/10.1127/0078-0421/2004/0040-0073.

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26

Claoué-Long, J. C., P. J. Jones, J. Roberts y S. Maxwell. "The numerical age of the Devonian-Carboniferous boundary". Geological Magazine 129, n.º 3 (mayo de 1992): 281–91. http://dx.doi.org/10.1017/s0016756800019221.

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AbstractThe SHRIMP ion microprobe has been used to date zircons in a 1 cm thick bentonite located in the Hasselbachtal auxiliary global stratotype section through the Devonian-Carboniferous boundary in Germany, and a tuff located at a similar biostratigraphic level in Australia. Multiple replicate analyses have yielded indistinguishable ages, and indicate 353.2±4.0 Ma (2σ) as the age of the boundary. Obtaining an age for the boundary in the German reference section depended on the ability of SHRIMP to date a small sample and to target small areas of structurally complex zircons. Future refinements of the age of this boundary may depend on re-analysis of this uniquely placed bentonite, and this highlights the value of defining biostratigraphic stratotypes in the vicinity of known dateable horizons.
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27

Diedrich, C. y E. W. A. Mulder. "A new record of Clidastes (Squamata, Mosasauridae) from the Upper Campanian of the Münster Basin (NW Germany)". Netherlands Journal of Geosciences - Geologie en Mijnbouw 83, n.º 1 (marzo de 2004): 67–71. http://dx.doi.org/10.1017/s0016774600020473.

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AbstractFrom Upper Campanian turbiditic marls at Beckum in the Münster Basin (NW Germany) the anterior portion of a mosasaurid premaxilla with abutting fragments of the left and right maxilla is described and referred to the genus Clidastes. It shows the process of tooth replacement very well. This taxon is recorded for the first time from Germany. Clidastes co-existed in central Europe with other mosasaurids such as representatives of the genus Leiodon and Mosasauridae indet.
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28

Bauer, Wilfried. "ISAES IX, Potsdam, Germany, September 8-12, 2003". Gondwana Research 7, n.º 2 (abril de 2004): 636–37. http://dx.doi.org/10.1016/s1342-937x(05)70818-2.

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29

Heinrichs, Gerold y Peter Udluft. "Natural arsenic concentrations in groundwaters in Germany with reference to aquifer geology". Zeitschrift der Deutschen Geologischen Gesellschaft 147, n.º 4 (23 de enero de 1997): 519–30. http://dx.doi.org/10.1127/zdgg/147/1997/519.

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30

Rose, J. "Tertiary and Quaternary geology of the Saale–Elbe region of eastern Germany". Quaternary Science Reviews 21, n.º 11 (mayo de 2002): 1241. http://dx.doi.org/10.1016/s0277-3791(02)00020-3.

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31

Bitner, Maria y Andreas Kroh. "First record of the genus Bronnothyris (Brachiopoda: Megathyrididae) from the Oligocene of the Mainz Basin (Germany)". Geologica Carpathica 62, n.º 3 (1 de junio de 2011): 203–9. http://dx.doi.org/10.2478/v10096-011-0017-8.

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First record of the genusBronnothyris(Brachiopoda: Megathyrididae) from the Oligocene of the Mainz Basin (Germany)The genusBronnothyris, with the type speciesTerebratula bronniiRoemer, 1841, was erected for thoseArgyrothecaspecies that have septal flanges extended ventrally from the dorsal valve. Four other Late Cretaceous and one Early Paleocene species were attributed to this genus (i.e.Argyrotheca coniunctaSteinich, 1965,A. lacunosaSteinich, 1965,A. obstinataSteinich, 1965,A. stevensisNielsen, 1928 andA. rugicostaZelinskaya, 1975). After examination of Oligocene material from Waldböckelheim, Mainz Basin, Germany we transfer the speciesArgiope subradiataSandberger, 1862 into the genusBronnothyris. This new combination extends the stratigraphic range ofBronnothyrisinto the Oligocene.
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32

Rowland, Stephen. "The Life and Geological Writings of the 'Father of Russian Science': Mikhail Lomonosov". Earth Sciences History 32, n.º 1 (1 de enero de 2013): 86–101. http://dx.doi.org/10.17704/eshi.32.1.w41v482666805150.

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Eighteenth-century Russian polymath Mikhail Lomonosov (1711-1765) is a highly celebrated and symbolically important figure in Russian culture, but he is not well known outside of Russia. In this paper I review his biography, his contributions to geology, and the key influences on his geological writings. He spent his youth on the coast of the White Sea, near the Arctic Circle, working with his father, who was a fisherman and merchant. This experience helped him to become a keen observer of natural phenomena. At age nineteen he traveled to Moscow, falsely claimed that he was the son of a nobleman, and talked his way into the Slavo-Graeco-Latin Academy. He excelled as a student and was chosen to continue his studies at the university in St Petersburg. From there he was one of three Russian students chosen to spend several years studying in Germany, primarily to learn about mining and the extraction of metals from ore. Lomonosov's four-and-a-half years in Germany were critical to his development as a scholar and scientist, immersing him in contemporary European knowledge and epistemology. After Lomonosov returned to the St Petersburg Academy of Sciences and Arts in 1741, he worked his way up the academic ladder, eventually becoming professor of chemistry, but it was not a smooth and steady climb. At one point he was under house arrest for eight months for rowdy conduct and discourteous behavior. Lomonosov made significant contributions to many fields of science. He wrote several geological publications, the most significant of which is On the Strata of the Earth (1763), which became available in German only in 1961, and in English only in 2012. Lomonosov's work in geology was motivated by his desire to promote economic development in Russia through the extraction of mineral resources, together with a deep curiosity about natural history.
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33

Balega, A., S. Vyzhva y M. Kurylo. "INSTITUTIONAL PROVISION OF GEOLOGICAL STUDY AND USE OF SUBSOIL: NATIONAL AND INTERNATIONAL EXPLORATION". Visnyk of Taras Shevchenko National University of Kyiv. Geology, n.º 4 (83) (2018): 63–72. http://dx.doi.org/10.17721/1728-2713.83.09.

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The national experience of institutional support for the study and use of subsoil are defined. The subjects of interaction in the sphere of geological mining use are defined, the mechanism of interaction is shown. The institutional provision of the study and use of subsoil is divided into three blocks of influence: institutions of general competence, inter-sectoral institutions of special competence and sectoral institutions of special competence. The role of the State Service of Geology and Mineral Resources of Ukraine in the system of institutional support of geological study and use of subsoil is determined. The structure of the State Service of Geology and Mineral Resources of Ukraine was systematized and the basic functions and directions of activity are defined. It is revealed that state financing of development of mineral base of Ukraine takes place through the system of enterprises and organizations belonging to the State Service of Geology and Mineral Resources of Ukraine. The structure and features of geological services in Germany, Poland and Australia were investigated. In the course of this analysis, a number of typical and a number of distinctive functions were identified for the geological services of the above mentioned countries. The State Service of Geology and Mineral Resources of Ukraine does not provide a number of key and progressive functions in the field of geological study and use of subsoil, such as: monitoring the state of the market of mineral resources, popularization of the mineral raw materials complex and enhancement of the investment attractiveness of the mineral base of Ukraine. It is concluded that for the introduction of foreign experience, changes should be made to the structure of the State Service of Geology and Mineral Resources of Ukraine. The study of the functional experience and the role of geological services in Australia and Germany testify to the effectiveness of regional geological services in the development of mineral base of these countries. Since the decentralization process in Ukraine has not been completed, experience in providing broad powers to local government bodies, a mineral base cannot be easy implemented.
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34

Morawietz, Sophia, Moritz Ziegler y Karsten Reiter. "An Open-Access Stress Magnitude Database for Germany". Safety of Nuclear Waste Disposal 1 (10 de noviembre de 2021): 71–72. http://dx.doi.org/10.5194/sand-1-71-2021.

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Abstract. The stress field in the Earth's crust plays a central role in the site-selection process for a deep geological repository for high-level nuclear waste. Site selection and construction planning must take into account several factors that are influenced by the stress state. These include the excavation damage zone, the hydraulic permeability of the host rock, the self-sealing capacity, the effects of seismic events and the possible reactivation of faults as migration pathways for fluids and radionuclides. Likewise, the initial stress state is of central importance for the long-term studies to prove site safety over 1 Ma. To obtain a continuous description of the current 3D stress state, 3D geomechanical numerical models are used. These models have to be calibrated with data on stress magnitudes to obtain robust predictions. One of the central goals of the SpannEnD project (Spannungsmodell Endlagerung Deutschland, http://www.spannend-projekt.de, last access: 31 October 2021) was to build the first comprehensive and publicly accessible stress magnitude database for Germany, including a quality ranking of the data compiled from different methods. This database is the logical extension of the database of the World Stress Map project, in which so far only information on stress orientations and the stress regime has been compiled systematically. We present this first compilation of stress magnitude data published and made available by Morawietz et al. (2020). The stress data density is generally low and heterogeneous, so that a model calibration at the scale of a site model is not possible. Therefore, the main objective of the SpannEnD project is to develop a 3D geomechanical numerical model for the whole of Germany. The resulting 3D stress field will provide the basis for regional and local models in a later phase of the site selection process. Details on this are presented in three complementary contributions in this symposium by Reiter et al., Röckel et al. and Ahlers et al. The new Geology Data Act (Geologie-Datengesetz) now allows access to considerably more data, which will be incorporated into an update of the database after assessment according to the defined quality criteria. This database extension will improve the reliability of the predictions of the geomechanical models on different spatial scales.
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35

Meyer, W. y J. Stets. "Pleistocene to Recent tectonics in the Rhenish Massif (Germany)". Netherlands Journal of Geosciences - Geologie en Mijnbouw 81, n.º 2 (agosto de 2002): 217–21. http://dx.doi.org/10.1017/s0016774600022460.

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AbstractUplift of the Rhenish Massif can be demonstrated by means of the stream-made river terrace system that accompanies the Rhine river and its tributaries along their way through or within this part of the Variscan fold and thrust belt. The height difference between a former valley floor, especially that of the Younger ‘Hauptterrasse’ (Main Terrace), and the recent one allows to quantify the uplift by the amount of downcutting erosion. The uplift velocity increased just after theBRUNHES / MATUYAMAboundary, i.e. about 0.8 Ma B.R Since that time, a domal uplift of more than 250 m is documented in the eastern Hunsriick and in the south-eastern Eifel. The area of this maximum height anomaly is situated just between the East-and West-Eifel Quaternary volcanic districts. Thus, causal connections are supposed. The domai uplift is affected by normal faulting partly inherited since Tertiary rifting.
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36

Wilmsen, Markus J. "The Cenomanian of Hoppenstedt, northern Germany a Subhercynian key section revisited". Newsletters on Stratigraphy 40, n.º 3 (22 de diciembre de 2004): 209–30. http://dx.doi.org/10.1127/0078-0421/2004/0040-0209.

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37

Marambio, Helena-Ulrike. "Germany". Statelessness & Citizenship Review 5, n.º 1 (11 de agosto de 2023): 105–11. http://dx.doi.org/10.35715/scr5001.119.

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38

Christensen, W. K. "Belemnocamax boweri Crick, an unusual belernnite from the Cenornanian of northwest Germany and eastern England". Bulletin of the Geological Society of Denmark 40 (3 de junio de 1993): 157–66. http://dx.doi.org/10.37570/bgsd-1993-40-06.

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A small population of Be/emnocamax boweri Crick, 1910 from the Lower Middle Cenomanian primus bed in the limestone pit at Wunstorf west of Hannover (NW Germany) is studied by biometrical methods in order to analyse the variation of critical characters. The monotypic Belemnocamax differs from all other Upper Cretaceous belemnitellids by the small size of the guard, which is conical in ventral and lateral views, and by ha"'.ing a long, deep, and broad ventral groove. B. boweri is very rare and has only been recorded from eastern England and northwest Germany, where it occurs in the Lower Middle Ceno­manian. The ancestry of this genus is unknown.
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39

Christensen, Walter Kegel. "Gradualistic evolution in Belemnitella from the middle Campanian of Lower Saxony, NW Germany". Bulletin of the Geological Society of Denmark 47 (11 de septiembre de 2000): 135–63. http://dx.doi.org/10.37570/bgsd-2000-47-10.

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Nine samples of the Belemnitella lineage, including the uppermost Lower and lower Upper Campanian B. mucronata and the uppermost lower Upper Campanian B. misburgensis sp. nov., from the expanded uppermost Lower and lower Upper Campanian succession of the Lehrte West Synclinee east of Hannover, Lower Saxony, northern Germany have been subjected to univariate and bivariate statistical analyses. The succession consists of monotonous marly limestones and calcareous marls, which were deposited during 4–5 m.y. in a fairly stable environment. Based on superficial resemblance alone the nine samples are nearly identical, but trends have been recognized in the morphological characters when treated quantitatively. Three characters, the length from the apex to the protoconch, the slenderness of the guard and the alveolar angle, show evolutionary reversals (socalled zig-zag evolution) with net decreases or increases. The Schatzky distance shows stasis in B. mucronata and decreases in B. misburgensis sp. nov. The fissure angle displays unidirectional evolution and increases gradually. These morphological changes are interpreted as long term phyletic gradualism, although this model of evolution has almost universally been depicted as one of unidirectional change. B. misburgensis sp. nov. is closely allied to B. mucronata (its ancestor), but differs in its slightly smaller and more slender guard, in addition to its smaller Schatzky distance and larger fissure angle. B. praecursor is recorded from the uppermost five metres of the Lower Campanian, and this is the first record of this species from the highest Lower Campanian of northern Germany. The uppermost Lower and Lower Upper Campanian belemnite assemblages of the Misburg/Höver area in northern Germany are reviewed. The Upper Campanian Belemnitella successions of Norfolk in England, the Maastricht-Liège district in The Netherlands and Belgium, the Mons Basin in southern Belgium, Scania in southern Sweden and the Misburg-Höver area in northwest Germany are compared and contrasted.
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40

Matthews, D. H. "DEKORP-Atlas: Deep-seismic reflection profiles from Germany". Marine and Petroleum Geology 9, n.º 1 (febrero de 1992): 108–9. http://dx.doi.org/10.1016/0264-8172(92)90011-3.

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41

Wolfgramm, M., A. Seibt, S. Hurter y G. Zimmermann. "Origin of geothermal fluids of Permo-Carboniferous rocks inthe NE German basin (NE Germany)". Journal of Geochemical Exploration 78-79 (mayo de 2003): 127–31. http://dx.doi.org/10.1016/s0375-6742(03)00133-x.

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42

Christensen, Walter Kegel, Jake M. Hancock y William James Kennedy. "The base of the Maastrichtian". Bulletin of the Geological Society of Denmark 47 (31 de diciembre de 2000): 81–85. http://dx.doi.org/10.37570/bgsd-2000-47-06.

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At the Brussels Symposium on Cretaceous Stage Boundaries in 1995, the Maastrichtian Working Group decided to recommend the first occurrence of the ammonite Pachydiscus neubergicus in the Tercis quarry near Dax in the Landes, southwest France as the boundary stratotype for the base of the Maastrichtian stage. On the basis of the echinoid genus Echinocorys the Campanian-Maastrichtian boundary beds of Tercis are correlated with the succession in north Norfolk, England, which in turn is correlated with the succession at Kronsmoor, northwest Germany on the basis of belemnites and brachiopods. If the possible correlation between Tercis and northwest Germany is true, the P. neubergicus and Belemnella lanceolata standards for the base of the Maastrichtian stage are not separated by more than 0.2 m.y.
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43

Franzen, Jens Lorenz. "First fossil primates from Eckfeld Maar, Middle Eocene (Eifel, Germany)". Eclogae Geologicae Helvetiae 97, n.º 2 (agosto de 2004): 213–20. http://dx.doi.org/10.1007/s00015-004-1115-8.

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44

Korn, D. "Early Carboniferous (Mississippian) calciturbidites in the northern Rhenish Mountains (Germany)". Geological Journal 43, n.º 2-3 (2008): 151–73. http://dx.doi.org/10.1002/gj.1100.

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45

ROSE, EDWARD P. F. "MILITARY GEOLOGY: AN AMERICAN TERM OF WORLD WAR I RE-DEFINED FOR THE BRITISH ARMY AT THE END OF WORLD WAR II". Earth Sciences History 42, n.º 2 (1 de julio de 2023): 291–326. http://dx.doi.org/10.17704/1944-6187-42.2.291.

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ABSTRACT The term ‘military geology’, translated from German after earlier use in French and Spanish publications, entered the English language via American publications from 1917 onwards, initially after the USA entered World War I. It was widely used in the USA and, in direct or indirect translation, in several European countries additional to Germany and Austria thereafter, but not in the United Kingdom—although military applications of geology had been perceived and utilized by the British Army for much of the previous century. However, the term was used and its scope defined on the basis of operational experience at a meeting in Brussels on 28 February to 1 March 1945 as World War II drew to an end, a meeting seemingly unique for the War in that it comprised five ‘British’ geologist officers of field rank: the South African Major Gordon Lyall Paver, English Major Frederick William Shotton, Australian-born but Canadian-educated English Major John Leonard Farrington, English Squadron Leader John Francis Kirkaldy, and Welsh Major David Ronald Arthur Ponsford. Their purpose was to review wartime use of ‘military geology’ in the British Army, and to make recommendations for a more efficient British military geological service in the future, especially in the Far East after the war in Europe entered its final phase. The meeting generated a four-page closely-typed unpublished ‘Memorandum: Military geology in the British services’ (now preserved in England in the Lapworth Museum at the University of Birmingham and in The National Archives, Kew, near London). This included a very brief summary of the British Army’s deployment of geologists within western Europe, East Africa, the Middle East, North Africa and the Mediterranean region, and India. Those present brought together long experience from all these campaign areas except India (and the Far East in general). That deficiency was made good later in the year, on 7 December 1945, when Eric J. Bradshaw, Superintending Geologist of the Strategic Branch of the Geological Survey of India, completed an 81-page typed unpublished ‘Military geology: Memorandum of post-war policy’ (accessible in England at Birmingham, at Kew, and at the British Geological Survey, Keyworth). This with its 23 pages of appendices records details of wartime work in India and discussions held by the author there and in the United Kingdom following the end of hostilities in Europe on 8 May 1945. It re-defines the scope of ‘military geology’ for British armed forces in terms of water (resources, floods and drainage), stone and miscellaneous mineral resources, soils, engineering projects (reconnaissance, stability and excavations), terrain, ‘photo-geology’ and several miscellaneous applications. The memorandum proposed a grandiose organization of 151 geologist officers plus ancillary staff for British military geology postwar. That organizational scheme was not adopted—but by 1945 the term ‘military geology’ had clearly extended from American to significant British use.
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46

Hoppe, Andreas, Stefan Lang, Christian Lerch y Oswald Marinoni. "Geology and a spatial decision support system for the surroundings of urban areas: An example from southern Hesse (Germany)". Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 157, n.º 1 (1 de enero de 2006): 135–45. http://dx.doi.org/10.1127/1860-1804/2006/0157-0135.

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47

Seo, Jungil. "The Formation of the German Literary Market and Translation Industry since the 18th Century". Hankuk University of Foreign Studies Literature Studies 90 (31 de mayo de 2023): 9–30. http://dx.doi.org/10.22344/fls.2023.90.09.

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Historian Rolf Engelsing defined the late 18th century as “a transitional period from intensive book reading to extensive reading.” But in the German-speaking world, domestic books alone could not fully satisfy the public's desire for reading. This is because people's cultural interests and tastes had diversified and increased. Therefore, the publishing world turned its attention to foreign literature and publications and began to translate foreign literature extensively. Until the early 1820s, translations were extremely rare. However, German writers and intellectuals migrated abroad due to censorship, leading to the shrinking of the German-speaking publishing culture. This contradictory phenomenon led to the growth of the translation industry in Germany, and the activities of translation factories were particularly active.
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48

Grube, F. y Th Voll­mer. "Der geologische Bau pleistozaner Inlandgletschersedimente Norddeutschlands". Bulletin of the Geological Society of Denmark 34 (31 de mayo de 1985): 13–25. http://dx.doi.org/10.37570/bgsd-1985-34-02.

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The geologic structure and genetic aspects of inland galcier sediments are described on examples from northern Germany. Different types of structures are demonstrated ranging from slight undulation to in­tense subglacial folding and shearing. Inland glacier sediments are called all deposits laid down and/or de­formed by inland glaciers. These sediments resting on glacially undeformed basement include lodgement till (at top) and below of it shear till, melt-out and deformation till. A fundamental tool of modern till stratigraphy is the knowledge of the geologic structure more than are petrography and geochemistry of moraines at present.
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49

Brandes, Christian, Thomas Plenefisch, David C. Tanner, Nicolai Gestermann y Holger Steffen. "Evaluation of deep crustal earthquakes in northern Germany - Possible tectonic causes". Terra Nova 31, n.º 2 (22 de febrero de 2019): 83–93. http://dx.doi.org/10.1111/ter.12372.

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50

Zolitschka, Bernd, Achim Brauer, Jörg F. W. Negendank, Hagen Stockhausen y Andreas Lang. "Annually dated late Weichselian continental paleoclimate record from the Eifel, Germany". Geology 28, n.º 9 (2000): 783. http://dx.doi.org/10.1130/0091-7613(2000)28<783:adlwcp>2.0.co;2.

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