Добірка наукової літератури з теми "Glacimarine"
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Статті в журналах з теми "Glacimarine"
Rosa, Kátia Kellem da, Rosemary Vieira, and Jefferson Cardia Simões. "Variabilidade do Processo de Descarga de Água de Degelo Glacial para o Ambiente Glacimarinho da Enseada Martel, ilha Rei George, Antártica (Variability of Water Discharge Process of Melting Ice Environment Glacimarinho of Martel Inlet, Rei George...)." Revista Brasileira de Geografia Física 4, no. 4 (January 22, 2012): 837. http://dx.doi.org/10.26848/rbgf.v4i4.232741.
Повний текст джерелаPowell, Ross D. "Modern Glacimarine Environments." Episodes 10, no. 1 (March 1, 1987): 23–25. http://dx.doi.org/10.18814/epiiugs/1987/v10i1/010.
Повний текст джерелаGilbert, Robert. "Rafting in glacimarine environments." Geological Society, London, Special Publications 53, no. 1 (1990): 105–20. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.06.
Повний текст джерелаDowdeswell, Julian A. "Processes of glacimarine sedimentation." Progress in Physical Geography: Earth and Environment 11, no. 1 (March 1987): 52–90. http://dx.doi.org/10.1177/030913338701100103.
Повний текст джерелаDomack, E. W. "Biogenic facies in the Antarctic glacimarine environment: Basis for a polar glacimarine summary." Palaeogeography, Palaeoclimatology, Palaeoecology 63, no. 4 (February 1988): 357–72. http://dx.doi.org/10.1016/0031-0182(88)90105-8.
Повний текст джерелаAndrews, John T., J. A. Dowdeswell, and J. D. Scourse. "Glacimarine Environments: Processes and Sediments." Arctic and Alpine Research 23, no. 4 (November 1991): 456. http://dx.doi.org/10.2307/1551688.
Повний текст джерелаMcCarroll, Danny. "Glacimarine Environments: Processes and Sediments." Holocene 2, no. 1 (March 1992): 93. http://dx.doi.org/10.1177/095968369200200117.
Повний текст джерелаPERSSON, KÄRSTIN MALMBERG. "Glacimarine environments: Processes and sediments." Boreas 20, no. 2 (January 16, 2008): 190. http://dx.doi.org/10.1111/j.1502-3885.1991.tb00307.x.
Повний текст джерелаKehrl, Laura M., Robert L. Hawley, Ross D. Powell, and Julie Brigham-Grette. "Glacimarine sedimentation processes at Kronebreen and Kongsvegen, Svalbard." Journal of Glaciology 57, no. 205 (2011): 841–47. http://dx.doi.org/10.3189/002214311798043708.
Повний текст джерелаÓ Cofaigh, C., K. A. Hogan, J. A. Dowdeswell, and K. Streuff. "Stratified glacimarine basin-fills in West Greenland fjords." Geological Society, London, Memoirs 46, no. 1 (2016): 99–100. http://dx.doi.org/10.1144/m46.83.
Повний текст джерелаДисертації з теми "Glacimarine"
Hildick, Alice. "Natural gamma activities in glacimarine sediments correlations with terrestrial source data /." [Gainesville, Fla.] : University of Florida, 2006. http://purl.fcla.edu/fcla/etd/UFE0017927.
Повний текст джерелаStreuff, Katharina Teresa. "Glacimarine sedimentary processes and products at fjord-terminating tidewater glacier margins." Thesis, Durham University, 2017. http://etheses.dur.ac.uk/12520/.
Повний текст джерелаCadman, Victoria Mary. "Glacimarine sedimentation and environments during Late Weichselian and Holocene in the Bellsund Trough and Van Keulenfjorden, Svalbard." Thesis, University of Cambridge, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.361437.
Повний текст джерелаWeinschütz, Luiz Carlos [UNESP]. "Estratigrafia de seqüências do Grupo Itararé (Neocarbonifero-Eopermiano) na região de Rio Negro (PR) - Mafra (SC)." Universidade Estadual Paulista (UNESP), 2006. http://hdl.handle.net/11449/102992.
Повний текст джерелаConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
O Grupo Itararé consiste de três grandes ciclos de afinamento ascendente, aos quais foi dado o status de Formação, nomeadas Lagoa Azul, Campo Mourão e Taciba. Essa é uma das bases para estabelecer a Estratigrafia de Seqüências do grupo; a outra é fornecida pelos ciclos climáticos do Quaternário, com os estágios glacial, deglacial e interglacial. A área de Rio Negro-Mafra apresenta uma excelente testemunhagem de poços que, junto a bons afloramentos, possibilita a construção de extensos perfis verticais de fácies; as fácies e ciclos de fácies formam a base para os Sistemas Deposicionais, cuja disposição espacial proporciona a construção das Seqüências. Cinco sistemas são identificados, Arenito, Diamictito, Folhelho, Varvito-Diamictito e Deglaciação, este formado por conglomerado, arenito, diamictito, varvito e folhelho. A estrutura de um Sistema de Deglaciação é a mesma do grande ciclo proposto para a estratigrafia do Grupo Itararé, exceto a mudança do varvito acima para ritmito da proposta litocronoestratigráfica. Foram identificadas cinco seqüências no Grupo Itararé. A seqüência Campo do Tenente, formada por dois espessos sistemas de varvitodiamictito, representando sistema glacicontinental correspondente a trato de mar alto. As seqüências Campo Mourão-I e II, iniciam com espessos sistemas Arenito de trato de mar baixo, seguindo-se sistemas Varvito-Diamictito (só para CM-I), de Deglaciação (trato transgressivo) e Folhelho marinho de mar alto (Siltito Mafra em CM-I, Folhelho Lontras em CM-II). As seqüências Taciba-I e II são mais complexas. TC-I começa com sistema Diamictito espesso, glacimarinho associado a mar alto?, seguido de sistema de Deglaciação. TC-II tem sistema Arenito canalizado de mar baixo, seguido de sistema de Deglaciação transgressiva e sistema Folhelho de mar alto.
The Itararé Group consists of three major fining-upward cycles, also considered as Formations: Lagoa Azul, Campo Mourão and Taciba. This is one of basis to establish the Sequence Stratigraphy for the group; the other one comes from the Quaternary model, where one can recognize three stages of a climatic cycle: glacial, deglacial, interglacial. The Rio Negro-Mafra area presents excellent cored wells and outcrops which allow to build extensive vertical facies logs; facies and facies cycle are the basis for Depositional Systems, whose spatial distribution allows to build Depositional Sequences. Five Systems are identified: Sandstone, Diamictite, Shale, Varvite- Diamictite and Deglaciation. The latter is formed by conglomerate, sandstone, diamictito, varvite and shale. The structure of the Deglaciation System is the same of one major cycle/Formation of Itararé Group, except for the varvite component, or rhythmite in the major cycle. Five sequences are recognized. The Campo do Tenente sequence is formed by two thick varvite-diamictite systems, from a glacicontinental system attributed to a highstand tract (the Campo do Tenente is a marginal equivalent of the marine Lagoa Azul/Roncador Bed). The Campo Mourão sequences (CM-I and CMII) begin with thick Sandstone systems from a lowstand tract; it follows Varvite- Diamictite (only for CM-I), Deglaciation and marine Shale systems, respectively from transgressive and highstand tracts (the CM-2 marine system is the thick Lontras Shale). Taciba Formation sequences TB-I and TB-II are more complex. TB-I starts with a thick, glaciomarine Diamictite system (highstand tract?), and is followed by Deglaciation system. TC-II starts with a channelized, lowstand Sandstone system, estuarine, deltaic and turbidite in origin; it follows the Deglatiation and marine Shale systems, from transgressive and highstand tracts.
Evans, J. "Late Weichselian and Holocene glacimarine sedimentation and environments in Kejser Franz Josephs Fjord and on the adjacent continental margin of East Greenland." Thesis, University of Cambridge, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.598894.
Повний текст джерелаWeinschütz, Luiz Carlos. "Estratigrafia de seqüências do Grupo Itararé (Neocarbonifero-Eopermiano) na região de Rio Negro (PR) - Mafra (SC) /." Rio Claro : [s.n.], 2006. http://hdl.handle.net/11449/102992.
Повний текст джерелаBanca: Maria Rita Caetano Chang
Banca: Antonio Roberto Saad
Banca: Paulo Roberto dos Santos
Banca: Oscar Rösler
Resumo: O Grupo Itararé consiste de três grandes ciclos de afinamento ascendente, aos quais foi dado o status de Formação, nomeadas Lagoa Azul, Campo Mourão e Taciba. Essa é uma das bases para estabelecer a Estratigrafia de Seqüências do grupo; a outra é fornecida pelos ciclos climáticos do Quaternário, com os estágios glacial, deglacial e interglacial. A área de Rio Negro-Mafra apresenta uma excelente testemunhagem de poços que, junto a bons afloramentos, possibilita a construção de extensos perfis verticais de fácies; as fácies e ciclos de fácies formam a base para os Sistemas Deposicionais, cuja disposição espacial proporciona a construção das Seqüências. Cinco sistemas são identificados, Arenito, Diamictito, Folhelho, Varvito-Diamictito e Deglaciação, este formado por conglomerado, arenito, diamictito, varvito e folhelho. A estrutura de um Sistema de Deglaciação é a mesma do grande ciclo proposto para a estratigrafia do Grupo Itararé, exceto a mudança do varvito acima para ritmito da proposta litocronoestratigráfica. Foram identificadas cinco seqüências no Grupo Itararé. A seqüência Campo do Tenente, formada por dois espessos sistemas de varvitodiamictito, representando sistema glacicontinental correspondente a trato de mar alto. As seqüências Campo Mourão-I e II, iniciam com espessos sistemas Arenito de trato de mar baixo, seguindo-se sistemas Varvito-Diamictito (só para CM-I), de Deglaciação (trato transgressivo) e Folhelho marinho de mar alto (Siltito Mafra em CM-I, Folhelho Lontras em CM-II). As seqüências Taciba-I e II são mais complexas. TC-I começa com sistema Diamictito espesso, glacimarinho associado a mar alto?, seguido de sistema de Deglaciação. TC-II tem sistema Arenito canalizado de mar baixo, seguido de sistema de Deglaciação transgressiva e sistema Folhelho de mar alto.
Abstract: The Itararé Group consists of three major fining-upward cycles, also considered as Formations: Lagoa Azul, Campo Mourão and Taciba. This is one of basis to establish the Sequence Stratigraphy for the group; the other one comes from the Quaternary model, where one can recognize three stages of a climatic cycle: glacial, deglacial, interglacial. The Rio Negro-Mafra area presents excellent cored wells and outcrops which allow to build extensive vertical facies logs; facies and facies cycle are the basis for Depositional Systems, whose spatial distribution allows to build Depositional Sequences. Five Systems are identified: Sandstone, Diamictite, Shale, Varvite- Diamictite and Deglaciation. The latter is formed by conglomerate, sandstone, diamictito, varvite and shale. The structure of the Deglaciation System is the same of one major cycle/Formation of Itararé Group, except for the varvite component, or rhythmite in the major cycle. Five sequences are recognized. The Campo do Tenente sequence is formed by two thick varvite-diamictite systems, from a glacicontinental system attributed to a highstand tract (the Campo do Tenente is a marginal equivalent of the marine Lagoa Azul/Roncador Bed). The Campo Mourão sequences (CM-I and CMII) begin with thick Sandstone systems from a lowstand tract; it follows Varvite- Diamictite (only for CM-I), Deglaciation and marine Shale systems, respectively from transgressive and highstand tracts (the CM-2 marine system is the thick Lontras Shale). Taciba Formation sequences TB-I and TB-II are more complex. TB-I starts with a thick, glaciomarine Diamictite system (highstand tract?), and is followed by Deglaciation system. TC-II starts with a channelized, lowstand Sandstone system, estuarine, deltaic and turbidite in origin; it follows the Deglatiation and marine Shale systems, from transgressive and highstand tracts.
Doutor
Книги з теми "Glacimarine"
Glacimarine environments. London: Geological Society, 1990.
Знайти повний текст джерелаA, Dowdeswell J., and Scourse James D, eds. Glacimarine environments: Processes and sediments. London: Geological Society, 1990.
Знайти повний текст джерелаDowdeswell, J. A. Glacimarine Environments: Processes and Sediments (Geological Society Special Publication). Amer Assn of Petroleum Geologists, 1990.
Знайти повний текст джерелаЧастини книг з теми "Glacimarine"
Stoker, Martyn S. "Glacimarine Environments/Geomorphic Provinces: Overview." In Glaciated Continental Margins, 169–72. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_67.
Повний текст джерелаCatto, Norm, Dori J. Kovanen, and Olav Slaymaker. "Quaternary Glacial, Glacimarine and Glacilacustrine History." In World Geomorphological Landscapes, 49–77. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35137-3_2.
Повний текст джерелаBell, Trevor, Alan K. Cooper, and Anders Solheim. "Glossary of Glacimarine and Acoustic Terminology." In Glaciated Continental Margins, 299–315. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_98.
Повний текст джерелаGeertsema, Marten, David M. Cruden, and John J. Clague. "The Landslide-Modified Glacimarine Landscape of the Terrace–Kitimat Area, BC." In World Geomorphological Landscapes, 349–61. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-44595-3_25.
Повний текст джерелаHesse, Reinhard, Ingo Klaucke, Saeed Khodabakhsh, and William B. F. Ryan. "Glacimarine Drainage Systems in Deep-sea: The NAMOC System of the Labrador Sea and its Sibling." In Glaciated Continental Margins, 286–89. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_95.
Повний текст джерелаBarrett, P. J. "Cenozoic Climate and Sea Level History from Glacimarine Strata off the Victoria Land Coast, Cape Roberts Project, Antarctica." In Glacial Sedimentary Processes and Products, 259–87. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304435.ch15.
Повний текст джерелаWhittington, Robert J., Carl Fredrik Forsberg, and Julian A. Dowdeswell. "Seismic and Side-Scan Sonar Investigations of Recent Sedimentation in an Ice-Proximal Glacimarine Setting, Kongsfjorden, North-West Spitsbergen." In Glaciated Continental Margins, 175–78. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_68.
Повний текст джерела"TEMPERATE GLACIMARINE SEQUENCE STRATIGRAPHY." In LATITUDINAL CONTROLS ON STRATIGRAPHIC MODELS AND SEDIMENTARY CONCEPTS, 208–9. Society for Sedimentary Geology, 2019. http://dx.doi.org/10.2110/sepmsp.108.15.
Повний текст джерелаOCOFAIGH, C. "Glacimarine Sediments and Ice-Rafted Debris." In Encyclopedia of Quaternary Science, 932–45. Elsevier, 2007. http://dx.doi.org/10.1016/b0-444-52747-8/00090-9.
Повний текст джерелаÓCofaigh, C. "GLACIAL LANDFORMS, SEDIMENTS | Glacimarine Sediments and Ice-Rafted Debris." In Encyclopedia of Quaternary Science, 932–45. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00090-9.
Повний текст джерелаТези доповідей конференцій з теми "Glacimarine"
Penkrot, Michelle L., John M. Jaeger, Leah J. LeVay, and Guillaume St-Onge. "MULTIVARIATE MODELING OF GLACIMARINE LITHOSTRATIGRAPHY USING SCANNING XRF AND MULTISENSORY CORE PROPERTIES VALIDATED WITH CT IMAGERY." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282907.
Повний текст джерела