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Journal articles on the topic 'Geochemistry – New York – Dresden'

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Published: 10 December 2022

Last updated: 29 January 2023

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1

YOSHITAKE, HIRAKU. "Macrocyrtus imomzodai Barševskis, 2016, a new synonym of Metapocyrtus (Orthocyrtus) orbiferoides Schultze, 1918 (Coleoptera: Curculionidae: Entiminae)." Zootaxa 4254, no. 3 (April 18, 2017): 375. http://dx.doi.org/10.11646/zootaxa.4254.3.5.

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Metapocyrtus (Orthocyrtus) orbiferoides Schultze, 1918 was described based on the female holotype collected from Ilocos Norte, North Luzon, Philippines. Since that time, it has been left unstudied for almost a century until I examined the holotype of M. (O.) orbiferoides in 2010 at Senckenberg Naturhistorische Sammlungen, Museum für Tierkunde, Dresden (SMTD). Recently, Barševskis (2016) described Macrocyrtus imomzodai based on two female specimens from Ilocos Norte, Luzon. Judging from the original description and dorsal and lateral habitus images, it is quite apparent that M. imomzodai is conspecific with M. (O.) orbiferoides. Here I propose a new synonymy based on these examinations. I thank Klaus-Dieter Klass, Olaf Jäger, Christian Schmidt, and Matthias Nuss (SMTD) for their support during my stay in Dresden. My thanks are also due to Steve R. Davis (American Natural History Museum, New York) and Naoko Nakahara (Tsukuba) for their help for preparing the manuscript.

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2

Barnett, Rosalind C. "Reviews: Women Over Forty: Visions and RealitiesGRAMBSJEAN DRESDEN. New York: Springer Publishing, 1989, 254 pp." Psychology of Women Quarterly 14, no. 4 (December 1990): 618–19. http://dx.doi.org/10.1177/036168439001400401.

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3

Viegas, G. M., L. G. Baise, and R. E. Abercrombie. "Regional Wave Propagation in New England and New York." Bulletin of the Seismological Society of America 100, no. 5A (September 20, 2010): 2196–218. http://dx.doi.org/10.1785/0120090223.

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4

Gradinskaitė, Vilma. "In Search of Missing Collection: The Case of Artist Albert Rappaport." Art History & Criticism 17, no. 1 (November 15, 2021): 31–42. http://dx.doi.org/10.2478/mik-2021-0003.

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Summary The artist Albert Rappaport was born in Anykščiai in 1898. In 1911, the family emigrated to New York. Rappaport became an American citizen in 1925 and began to travel widely. He studied fine art in New York, Paris, Dresden and Munich. He visited South America, Africa and traveled extensively through Europe (1925–1927, 1933, 1937–1939), returning to the United States now and again. The artist participated in several dozen exhibitions. He showed his work in Paris, Rome, Florence, Barcelona, Palma de Mallorca, Copenhagen, Mexico City, Havana, New York, Calgary and Montreal, in addition to his solo exhibitions in 1937 in Warsaw and Vilnius, and in Kaunas, Riga and Tallinn in 1938. After Rappaport’s death, in March 17, 1969 in Montreal, his collection of artworks disappeared and has thus far not been found. To date, two of his painted portraits are known to exist – one belongs to the private collection of Jonathan C. Rappaport, another is on display at the Jewish Public Library in Montreal.

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5

Whelan, J. F., R. O. Rye, W. F. Delorraine, and H. Ohmoto. "Isotopic geochemistry of the mid-Proterozoic evaporite basin; Balmat, New York." American Journal of Science 290, no. 4 (April 1, 1990): 396–424. http://dx.doi.org/10.2475/ajs.290.4.396.

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6

Seifert, Karl E., Robert F. Dymek, Philip R. Whitney, and Larry A. Haskin. "Geochemistry of massif anorthosite and associated rocks, Adirondack Mountains, New York." Geosphere 6, no. 6 (December 2010): 855–99. http://dx.doi.org/10.1130/ges00550.1.

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7

Whitney, Philip R., and James F. Olmsted. "Geochemistry and origin of albite gneisses, northeastern Adirondack Mountains, New York." Contributions to Mineralogy and Petrology 99, no. 4 (August 1988): 476–84. http://dx.doi.org/10.1007/bf00371938.

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8

Lupulescu, M. V., J. Rakovan, G. W. Robinson, and J. M. Hughes. "FLUOROPARGASITE, A NEW MEMBER OF THE CALCIC AMPHIBOLES FROM EDENVILLE, ORANGE COUNTY, NEW YORK." Canadian Mineralogist 43, no. 4 (August 1, 2005): 1423–28. http://dx.doi.org/10.2113/gscanmin.43.4.1423.

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9

Mahon, Keith I. "The New “York” Regression: Application of an Improved Statistical Method to Geochemistry." International Geology Review 38, no. 4 (April 1996): 293–303. http://dx.doi.org/10.1080/00206819709465336.

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10

Helm, Jutta A. "Introduction: German Cities Between Globalization and Unification." German Politics and Society 16, no. 4 (December 1, 1998): 7–17. http://dx.doi.org/10.3167/104503098782486979.

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For more than a century, Germany has had a well-balanced systemof cities showcasing considerable variety in their social and physicalmake-up. It has lacked spectacular global cities like New York,Tokyo, or London. Instead, western cities include industrial citieslike those in the Rhine-Ruhr Valley and cities shaped by universitiesand research (Göttingen or Freiburg), media and publishing (Hamburg),culture and high-technology sectors (Munich), banking andfinance (Frankfurt/Main), wholesale trade and insurance (Cologneand Düsseldorf), as well as government and administration (Berlin,Bonn, and most state capitals). Dramatic social or economic crisesthat generate debates about urban decline have not happened.Thanks in part to effective urban governments, no German city hascome close to the near-collapse of American rustbelt cities duringthe early 1980s, or the fiscal meltdown of New York City in the1970s. Crime has been consistently lower and less violent, and theAmerican racial divide has no equivalent in German cities. East Germancities, while more unevenly developed, have been no less stable.East Berlin was the dominant center, linked to the industrialcities in the North (Rostock) and South (Leipzig, Halle, Dresden) bya rather creaky infrastructure.

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11

Leatherman, Stephen P. "Geomorphic and stratigraphic analysis of Fire Island, New York." Marine Geology 63, no. 1-4 (February 1985): 173–95. http://dx.doi.org/10.1016/0025-3227(85)90083-0.

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12

Rao, Usha, and Udo Fehn. "Sources and reservoirs of anthropogenic iodine-129 in western New York." Geochimica et Cosmochimica Acta 63, no. 13-14 (July 1999): 1927–38. http://dx.doi.org/10.1016/s0016-7037(99)00133-7.

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13

Browne, Kathleen M., and Robert V. Demicco. "Thrombolites of the lower devonian Manlius Formation of central New York." Carbonates and Evaporites 2, no. 2 (September 1988): 149–55. http://dx.doi.org/10.1007/bf03174314.

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14

Friedman, Gerald M. "Late Cambrian cabbage-head stromatolites from Saratoga Springs, New York, USA." Carbonates and Evaporites 15, no. 1 (March 2000): 37–48. http://dx.doi.org/10.1007/bf03175647.

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15

Grew, Edward S., Martin G. Yates, and William deLorraine. "Serendibite from the northwest Adirondack Lowlands, in Russell, New York, USA." Mineralogical Magazine 54, no. 374 (March 1990): 133–36. http://dx.doi.org/10.1180/minmag.1990.054.374.17.

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16

Warr, L. N., and R. Ferreiro Mählmann. "Recommendations for Kübler Index standardization." Clay Minerals 50, no. 3 (August 2015): 283–86. http://dx.doi.org/10.1180/claymin.2015.050.3.02.

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AbstractFollowing a round-table discussion at the Mid-European Clay Conference in Dresden 2014, new recommendations for illite ‘crystallinity’ Kübler index standardization have been agreed upon. The use of Crystallinity Index standards in the form of rock-fragment samples will be continued, along with the same numerical scale of measurement presented by Warr & Rice (1994). However, in order to be compatible with the original working definition of Kübler's (1967) anchizone, the upper and lower boundary limits of the Crystallinity Index Standard (CIS) scale are adjusted appropriately from 0.25°2θ and 0.42°2θ to 0.32°2θ and 0.52°2θ. This adjustment is based on an inter-laboratory correlation between the laboratories of Basel, Neuchâtel and the CIS scale. The details of this correction are presented in this first note, as discussed at the round-table meeting and will be further substantiated by a correlation program between CIS and former Kübler–Frey–Kisch standards.

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17

LANCASTER, P. J., B. FU, F. Z. PAGE, N. T. KITA, M. E. BICKFORD, B. M. HILL, J. M. McLELLAND, and J. W. VALLEY. "Genesis of metapelitic migmatites in the Adirondack Mountains, New York." Journal of Metamorphic Geology 27, no. 1 (January 2009): 41–54. http://dx.doi.org/10.1111/j.1525-1314.2008.00802.x.

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18

Lupulescu, M. V., J. Rakovan, M. D. Dyar, G. W. Robinson, and J. M. Hughes. "FLUORO-POTASSICHASTINGSITE FROM THE GREENWOOD MINE, ORANGE COUNTY, NEW YORK: A NEW END-MEMBER CALCIC AMPHIBOLE." Canadian Mineralogist 47, no. 4 (August 1, 2009): 909–16. http://dx.doi.org/10.3749/canmin.47.3.909.

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19

Desbois, G., J. Ingrin, N. T. Kita, J. W. Valley, and E. Deloule. "New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and 18O profiles." American Mineralogist 92, no. 4 (April 1, 2007): 453–59. http://dx.doi.org/10.2138/am.2007.2224.

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20

MEURER, S. "Women Over forty: Visions and realities, revised edition By Jean Dresden Grambs. New York: Springer, 1989. 254 pages. $38.95, hardcover; $25.95, softcover." Journal of Nurse-Midwifery 36, no. 6 (November 1991): 383–84. http://dx.doi.org/10.1016/0091-2182(91)90118-9.

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21

Scileppi, Elyse, and Jeffrey P. Donnelly. "Sedimentary evidence of hurricane strikes in western Long Island, New York." Geochemistry, Geophysics, Geosystems 8, no. 6 (June 2007): n/a. http://dx.doi.org/10.1029/2006gc001463.

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22

Friedman, Gerald M. "Erratum to: Late cambrian cabbage-head stromatolites from Saratoga Springs, New York, USA." Carbonates and Evaporites 15, no. 2 (September 2000): 195. http://dx.doi.org/10.1007/bf03175826.

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23

Jaffe, Howard W., Leo M. Hall, and Howard T. Evans. "Wagnerite with isokite from the Benson Mines, west-central Adirondack Highlands, New York." Mineralogical Magazine 56, no. 383 (June 1992): 227–33. http://dx.doi.org/10.1180/minmag.1992.056.383.09.

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AbstractThe rare fluophosphate minerals wagnerite, ideally Mg2(PO4)F, and isokite, ideally CaMg(PO4)F, are intimately associated with magnetite-hematite deposits in sillimanite-, garnet-, and pyroxene-rich paragneisses and migmatites at the Benson Mines, near Star Lake in the west-central Adirondack Highlands of New York State. Coarsely crystalline wagnerite occurs in lenticular masses, typically 4 × 8 cm, delineated by sharply cross-cutting, sinuous, 2 cm-wide veins of fine-grained, fibrous to platy isokite and granular fluorapatite. These also penetrate transverse fractures across wagnerite lenses. Isokite formed from the introduction of Ca- and O-rich hydrothermal solutions into wagnerite. Both minerals are monoclinic: wagnerite crystallises in space group P21/a with a = 11.945, b = 12.717, c = 9.70 Å, β = 108.18°, V = 1400.2 Å3, D(calc) = 3.291 g/cm3 for Z = 16; isokite crystallises in space group A2/a with a = 6.909, b = 8.746, c = 6.518 Å, β = 112.20°, V = 364.7 Å3, D(calc) = 3.248 for Z = 4. Optical properties for wagnerite are: α = 1.5845, β = 1.5875, γ = 1.6010, 2V = 51°(calc.) disp = r < v weak, absorption α < β > γ with α = col., β = pale yel., γ = v. pale yel. For isokite only a mean index of refraction, n = 1.598, could be measured. Wet chemical analysis of wagnerite containing a calculated 11.4% of isokite as fine lamellae, gave the formula:

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24

Leger, Albert, Carolyn Rebbert, and Jim Webster. "Cl-rich biotite and amphibole from Black Rock Forest, Cornwall, New York." American Mineralogist 81, no. 3-4 (April 1, 1996): 495–504. http://dx.doi.org/10.2138/am-1996-3-423.

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25

Lupulescu, M. V., J. R. Chiarenzelli, and D. G. Bailey. "MINERALOGY, CLASSIFICATION, AND TECTONIC SETTING OF THE GRANITIC PEGMATITES OF NEW YORK STATE, USA." Canadian Mineralogist 50, no. 6 (December 1, 2012): 1713–28. http://dx.doi.org/10.3749/canmin.50.6.1713.

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26

Friedman, Gerald M. "Early ordovician microbial reef mounds of the tribes Hill formation, Mohawk Valley, New York." Carbonates and Evaporites 11, no. 2 (September 1996): 226–40. http://dx.doi.org/10.1007/bf03175641.

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27

Friedman, Gerald M. "Explosive bolide impact designates the Cambrian Explosion, terminating the Cambrian event in New York." Carbonates and Evaporites 22, no. 2 (September 2007): 178–85. http://dx.doi.org/10.1007/bf03176245.

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28

Więckowska, Katarzyna. "Between and Beyond Intersex and Transgender Studies: A Review of Transgender and Intersex: Theoretical, Practical, and Artistic Perspectives, Stefan Horlacher ed., New York: Palgrave Macmillan, 2016." Anglica Wratislaviensia 56 (November 22, 2018): 321–29. http://dx.doi.org/10.19195/0301-7966.56.20.

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This review assesses Transgender and Intersex: Theoretical, Practical, and Artistic Perspectives 2016, edited by Stefan Horlacher. Inspired by the international and interdisciplinary conference on “Transgender and Intersex in the Arts, Science and Society” that was held in 2012 in Dresden and that gathered researchers, activists, and artists working in transgender and intersex studies, the collection aims at mapping potential alliances between intersex and transgender positions, while acknowledging that the interests of transgender and intersex communities and researchers may be conflicting, if not at times contradictory. The volume adopts a non-hierarchical, multiperspectival, and interdisciplinary approach to examine a variety of issues related to gender variance and politics of recognition. Accordingly, the articles focus on those processes and texts that have played major roles in deconstructing and reconstructing gender identities during the late twentieth and early twenty-first centuries, and present analyses of legal and sociopolitical issues, theoretical perspectives and dilemmas, and literary and visual representations. The diverse topics and perspectives embrace the ethical framework of human rights, so as to inquire into the ways through which the lives and representations of marginalized groups can be improved.

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29

Fossen, Mickey C. Van, and Dennis V. Kent. "A Palaeomagnetic Study of 143 Ma Kimberlite Dikes In Central New York State." Geophysical Journal International 113, no. 1 (April 1993): 175–85. http://dx.doi.org/10.1111/j.1365-246x.1993.tb02538.x.

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30

Peck, W. H., and J. W. Valley. "Quartz-garnet isotope thermometry in the southern Adirondack Highlands (Grenville Province, New York)." Journal of Metamorphic Geology 22, no. 8 (October 2004): 763–73. http://dx.doi.org/10.1111/j.1525-1314.2004.00547.x.

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31

Parker, W. C., P. C. Ragland, and D. A. Textoris. "Controls on trace elements in the Ordovician Black River Group, New York, U.S.A." Chemical Geology 53, no. 1-2 (December 1985): 83–94. http://dx.doi.org/10.1016/0009-2541(85)90022-1.

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32

Kafka, Alan L., Ellyn A. Schlesinger-Miller, and Noel L. Barstow. "Earthquake activity in the greater New York City area: Magnitudes, seismicity, and geologic structures." Bulletin of the Seismological Society of America 75, no. 5 (October 1, 1985): 1285–300. http://dx.doi.org/10.1785/bssa0750051285.

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Abstract Earthquakes recorded by stations of the Lamont-Doherty seismic network in the greater New York City area are analyzed to determine magnitudes and the relationship between seismicity and geologic structures. Between 1974 and 1983, the configuration of stations in this region remained relatively stationary and the type of recording devices (visual drum recorders and 16-mm photographic recorders) did not change. This distribution of stations and recording devices allows for a uniform measurement of magnitudes and seismicity. Magnitudes of these earthquakes are determined by comparing amplitudes and signal duration measured from high-frequency (5 to 10 Hz) data recorded by the local network with mbLg and ML determined from data at frequencies near 1 Hz. During the period of time studied (nearly 10 yr), 61 earthquakes were located in this region, but none of these earthquakes exceeded 3.0 on the mbLg scale. The largest event (mbLg = 3.0) occurred in the Coastal Plain province of northern New Jersey. The magnitude threshold for uniform detection of events throughout this region during the period of time studied is estimated to be mbLg = 1.6. With events below this threshold removed from the catalog of network seismicity, we find that about half of the earthquakes studied occurred within 10 km of the Ramapo fault system. This fault system lies about 30 km northwest of New York City and has been interpreted by several investigators to be the most active fault system in the greater New York City area. However, earthquakes at least as large as those recorded near the Ramapo fault were located as far as 50 km from this fault (and within 20 km of New York City), in geologic structures that surround the Newark basin. While the Ramapo fault can by no means be ruled out as a possible source zone for earthquakes in the greater New York City area, the geologic structures associated with most (if not all) earthquakes in this region are still unknown. Thus, the cause of earthquakes in this region remains an enigma.

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33

Kolkas, Mossbah M., and Gerald M. Friedman. "Diagenetic history and geochemistry of the Beekmantown-Group dolomites (Sauk Sequence) of New York, USA." Carbonates and Evaporites 13, no. 1 (March 1998): 69–85. http://dx.doi.org/10.1007/bf03175436.

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34

Guo, Baiying, John E. Sanders, and Gerald M. Friedman. "Timing- and origin of dedolomite in upper Wappinger Group (Lower Ordovician) strata, southeastern New York." Carbonates and Evaporites 11, no. 1 (March 1996): 113–33. http://dx.doi.org/10.1007/bf03175790.

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35

Dorfler, K. M., R. J. Tracy, and M. J. Caddick. "Late-stage orogenic loading revealed by contact metamorphism in the northern Appalachians, New York." Journal of Metamorphic Geology 32, no. 1 (December 28, 2013): 113–32. http://dx.doi.org/10.1111/jmg.12061.

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36

JOHNSON, C. D., and W. D. CARLSON. "The origin of olivine-plagioclase coronas in metagabbros from the Adirondack Mountains, New York." Journal of Metamorphic Geology 8, no. 6 (November 1990): 697–717. http://dx.doi.org/10.1111/j.1525-1314.1990.tb00496.x.

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37

Florence, F. P., R. S. Darling, and S. E. Orrell. "Moderate pressure metamorphism and anatexis due to anorthosite intrusion, western Adirondack Highlands, New York." Contributions to Mineralogy and Petrology 121, no. 4 (October 17, 1995): 424–36. http://dx.doi.org/10.1007/s004100050107.

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38

Friedman, G. M., and D. J. Schultz. "Precipitation of vaterite (CaCO3) during oil field drilling." Mineralogical Magazine 58, no. 392 (September 1994): 401–8. http://dx.doi.org/10.1180/minmag.1994.058.392.05.

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AbstractVaterite, a CaCO3 polymorph, is a rare mineral that is said to be metastable under all known conditions. According to the literature, vaterite precipitated from carbonate solution recrystallizes spontaneously to calcite or aragonite. Yet vaterite has been identified in hard tissues of organisms, in gallstones, in contact metamorphic aureoles, in zones of thermal metamorphism, in a meteorite, and in cone-in-cone concretions. Newly precipitated vaterite has formed at the expense of carbonate rock in drilling fluids in wells of New York, Michigan, Nevada, Texas, and New Zealand. Petrographic examination reveals a light brown core of Ca3SiO5 surrounded by a colourless rim of vaterite. The δ18OPDB of New York vaterite is −12.4‰ and that of the Michigan vaterite is −17.6‰, which reflect the oxygen isotopic composition of meteoric freshwater used in drilling. The δ13CPDB value of −19.2‰ for New York vaterite and that of −17.6‰ for Michigan vaterite suggest that natural gas dissolved original carbonate in the subsurface. Drilling records from both wells indicate that natural gas was released into the drilling muds from the formations exposed at the time vaterite was encountered. Crossplots of the oxygen and carbon isotopic ratios overlap those of spurrite rocks in thermal metamorphic zones in Israel. A C-14 radiocarbon analysis of the Michigan vaterite gave an age of 953±39 yr. BP. 88.8±0.6% is modern carbon and 11.2% is dead carbon. Hence this carbon, and therefore the vaterite, is essentially modern. A sample of the New York vaterite yielded a modern age.

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39

GERDES, M. L., and J. W. VALLEY. "Fluid flow and mass transport at the Valentine wollastonite deposit, Adirondack Mountains, New York State." Journal of Metamorphic Geology 12, no. 5 (September 1994): 589–608. http://dx.doi.org/10.1111/j.1525-1314.1994.tb00045.x.

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40

Whitney, Philip R. "Charnockites and granites of the western Adirondacks, New York, USA: a differentiated A-type suite." Precambrian Research 57, no. 1-2 (June 1992): 1–19. http://dx.doi.org/10.1016/0301-9268(92)90092-3.

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41

OLSON, K. E. "The Petrology and Geochemistry of Mafic Igneous Rocks in the Anorthosite-Bearing Adirondack Highlands, New York." Journal of Petrology 33, no. 2 (April 1, 1992): 471–502. http://dx.doi.org/10.1093/petrology/33.2.471.

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42

Cressey, G., J. Spratt, and B. A. Cressey. "Electron and X-ray petrography of an unusual serpentine from the Tilley Foster Mine, Brewster, New York." Canadian Mineralogist 31, no. 2 (June 1, 1993): 447–58. http://dx.doi.org/10.3749/1499-1276-31.2.447.

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43

Windley, B. F. "L. D Ashwal. Anorthosites. Berlin, Heidelberg and New York (Springer Verlag), 1993. xix + 422 pp. Price DM168.00." Mineralogical Magazine 58, no. 390 (March 1994): 178–79. http://dx.doi.org/10.1180/minmag.1994.058.390.24.

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44

Peck, W. H., M. E. Bickford, J. M. McLelland, A. N. Nagle, and G. J. Swarr. "Mechanism of metamorphic zircon growth in a granulite-facies quartzite, Adirondack Highlands, Grenville Province, New York." American Mineralogist 95, no. 11-12 (November 1, 2010): 1796–806. http://dx.doi.org/10.2138/am.2010.3547.

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45

McLelland, James, Michael Hamilton, Bruce Selleck, Jonathan McLelland, Douglas Walker, and Suzanne Orrell. "Zircon U-Pb geochronology of the Ottawan Orogeny, Adirondack Highlands, New York: regional and tectonic implications." Precambrian Research 109, no. 1-2 (June 2001): 39–72. http://dx.doi.org/10.1016/s0301-9268(01)00141-3.

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46

Childs, Peter P., and Sethu Raman. "Observations and Numerical Simulations of Urban Heat Island and Sea Breeze Circulations over New York City." Pure and Applied Geophysics 162, no. 10 (June 21, 2005): 1955–80. http://dx.doi.org/10.1007/s00024-005-2700-0.

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47

Smith, Pamela H. "Court Culture in Dresden: From Renaissance to Baroque. By Helen Watanabe-O'Kelly. New York: Palgrave. 2002. Pp. xv + 310. 56 figs. $39.95. ISBN 0-333-98448-X." Central European History 37, no. 4 (December 2004): 593–96. http://dx.doi.org/10.1163/1569161043419280.

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48

Lupulescu, Marian V., John M. Hughes, Jeffrey R. Chiarenzelli, and David G. Bailey. "Texture, Crystal Structure, and Composition of Fluorapatites From Iron Oxide-Apatite (Ioa) Deposits, Eastern Adirondack Mountains, New York." Canadian Mineralogist 55, no. 3 (May 2017): 399–417. http://dx.doi.org/10.3749/canmin.1600057.

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49

Liogys and Jenkins. "Hornblende geothermometry of amphibolite layers of the Popple Hill gneiss, north-west Adirondack Lowlands, New York, USA." Journal of Metamorphic Geology 18, no. 5 (September 2000): 513–30. http://dx.doi.org/10.1046/j.1525-1314.2000.00271.x.

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STORM, L. C., and F. S. SPEAR. "Pressure, temperature and cooling rates of granulite facies migmatitic pelites from the southern Adirondack Highlands, New York." Journal of Metamorphic Geology 23, no. 2 (February 2005): 107–30. http://dx.doi.org/10.1111/j.1525-1314.2005.00565.x.

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