Relevant bibliographies by topics / Glacimarine

Academic literature on the topic 'Glacimarine'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Contents

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Glacimarine.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Glacimarine"

1

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.

Full text
Abstract:
A liberação da água estocada no sistema glacial depende da variabilidade da descarga de água de degelo pelas geleiras para o ambiente glacimarinho. Com o processo de retração das geleiras, torna-se importante o monitoramento destes processos. Neste trabalho, a dinâmica hidrológica de geleiras que drenam para a enseada Martel, ilha Rei George, Shetlands do Sul, Antártica, foi investigada através de informações do aporte de água de degelo para o ambiente glacimarinho. Foram realizadas mensurações de vazão no canal proglacial da geleira Wanda e análises da distribuição espacial dos fluxos de água de degelo das geleiras que drenam para a enseada através de técnicas de processamento de imagem ASTER. Resultados demonstram que esses processos liberam um grande fluxo de água de degelo dentro da circulação estuarina, tanto por fluxos em canais proglaciais, provenientes da fusão de geleiras de término terrestre, quanto das geleiras de maré. Esses podem refletir a variabilidade climática evidenciada na área de estudo. Dados demonstraram que há uma correlação direta entre a variabilidade da descarga de água de degelo, a profundidade do perfil do canal proglacial e o aumento da temperatura média do ar local. Assim, o uso desta metodologia possui potencial para o uso no desenvolvimento de modelos de monitoramento da variabilidade dos processos de estocagem de água de degelo. Flutuações nos fluxos de água de degelo podem acarretar mudanças ambientais na dinâmica glacial, na produção de sedimentos glaciais, no nível médio local do mar e nos níveis de salinidade no ambiente glacimarinho.Palavras chaves: estocagem hídrica, mudanças ambientais, descarga de água de degelo, ambiente glacimarinho, canais proglaciais Variability of Water Discharge Process of Melting Ice Environment Glacimarinho of Martel Inlet, Rei George Island, Antarctica ABSTRACTThe release of water storage in glacial system depends on meltwater discharge variability by glacimarine environment. With the glacial retreat, the monitor these processes become relevant for glaciological studies. In this work, the hydrological dynamic of the glaciers with flow for Martel inlet, King George Island, South Shetlands, Antarctica, was investigated through of meltwater contribution date for glacimarine environment. Was performed discharge measurements in proglacial channel at Wanda glacier and analyzed the spatial meltwater contribution of the glaciers in inlet through Aster image processing techniques. Results show that these processes release significantly meltwater flow for Martel inlet by proglacial channels, provided for proglacial terminus glaciers, and tidewater glaciers. These processes can be consequence of climatic variability evidenced in study area. Date show the correlation between the meltwater discharge variability, the proglacial channel profile depth and the air temperate increase. Thus, the application of methodology has potential for variability glacial water storage monitoring studies. Meltwater discharge fluctuations can provide environmental changes in glacial dynamic, glacial sediment yield, level sea and salinity levels in study area.Keywords: water storage, environmental change, melting water discharge, glacimarine environmental, proglacial channel
APA, Harvard, Vancouver, ISO, and other styles
2

Powell, Ross D. "Modern Glacimarine Environments." Episodes 10, no. 1 (March 1, 1987): 23–25. http://dx.doi.org/10.18814/epiiugs/1987/v10i1/010.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Gilbert, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Dowdeswell, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Domack, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Andrews, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

McCarroll, Danny. "Glacimarine Environments: Processes and Sediments." Holocene 2, no. 1 (March 1992): 93. http://dx.doi.org/10.1177/095968369200200117.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

PERSSON, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Kehrl, 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.

Full text
Abstract:
AbstractTidewater glaciers deposit sediment at their terminus, thereby reducing the relative water depth. Reduced water depth can lead to increased glacier stability through decreased rates of iceberg calving, glacier thinning and submarine melting. Here we investigate sedimentation processes at the termini of Kronebreen and Kongsvegen, Svalbard. We mapped the fjord floor bathymetry in August 2009 and calculate sedimentation rates based on our bathymetry and that from a similar study in 2005. A grounding-line fan is developing near the current position of the subglacial stream. An older, abandoned grounding-line fan that likely formed between ∼1987 and 2001 is degrading near the middle of the ice front. Our findings indicate that sediment gravity flows reduce the height of the sediment mound forming at the glacier terminus. The future impact of glacimarine sedimentation processes on glacier stability will depend on the net balance between the observed gravity flows and sediment deposition.
APA, Harvard, Vancouver, ISO, and other styles
10

Ó 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Glacimarine"

1

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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Streuff, Katharina Teresa. "Glacimarine sedimentary processes and products at fjord-terminating tidewater glacier margins." Thesis, Durham University, 2017. http://etheses.dur.ac.uk/12520/.

Full text
Abstract:
Tidewater glaciers terminate in the ocean and provide an important link between the terrestrial and marine realm, which makes them particularly vulnerable to both atmospheric and oceanographic changes. Tidewater glacier dynamics are affected by sea-level rise, which, in combination with ocean warming, can amplify glacier retreat. Most glaciers that drain the large contemporary ice sheets of Greenland and Antarctica are marine-terminating, fast-flowing outlets, and the dynamics of these glaciers have a large impact on ice sheet stability and sea level. Understanding how such glaciers have responded to climate change in the past therefore provides an important analogue for assessing current and future changes of the large ice sheets in Greenland and Antarctica. Fjords have proven to be very useful in this context, as their protected environment allows for the accumulation of thick, undisturbed sedimentary sequences, which enable the investigation of past ice sheet change at a high temporal resolution. This study uses multibeam swath-bathymetry, sub-bottom profiler data, and sediment cores from fjords in Spitsbergen and West Greenland to investigate the glacial landforms and sedimentary facies in front of fjord-terminating tidewater glaciers. The identified landform-sediment assemblages are compared to other High-Arctic fjords and are summarised in a new conceptual model. They are used to infer common sedimentary processes in glacimarine environments, to identify the factors controlling them, and to reconstruct Holocene regional ice dynamics. The results demonstrate that while the sedimentary processes are largely similar between the different regions, differences arise in the landform-sediment assemblages, even between adjacent fjords. This implies that glacier dynamics are not simply controlled by changes in the air or ocean temperatures, but can be highly variable in space and time.
APA, Harvard, Vancouver, ISO, and other styles
3

Cadman, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Weinschütz, 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.

Full text
Abstract:
Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2006-11-30Bitstream added on 2014-06-13T19:42:54Z : No. of bitstreams: 1 weinschutz_lc_dr_rcla.pdf: 1742525 bytes, checksum: 5b9c5ed9e9f54d4ef0daafc46b0439a4 (MD5)
Conselho 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.
APA, Harvard, Vancouver, ISO, and other styles
5

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.

Full text
Abstract:
The study outlines the glacimarine sedimentation patterns and processes and environments in the Kejser Franz Josephs Fjord and on the adjacent continental margin of East Greenland during the Late Weichselian and Holocene. A variety of techniques are adopted in the study in order to address the objectives outlined previously. The study is based on a suite of 8 cores from the mid to outer region of Kejser Franze Josephs Fjord, and the continental shelf and slope. Core analyses included i) logging (core and x-radiographs), ii) determination of grain size distribution, iceberg rafted debris and physical properties (water content, porosity, grain density), iii) determination of stable oxygen and carbon isotopes, iv) radiocarbon dating, and v) calculation of sedimentation and accumulation rates. Additionally, acoustic data is incorporated into the study to place the sediment cores within a regional context in terms of the sedimentation patterns and processes throughout the study area. The sedimentary record within the study dates back to the Late Weicheselian glaciation. The sedimentary record corresponding to the Late Weicheselian glaciation is confined to the continental slope, and partly the continental shelf. The nature, timing, extent and mechanisms of ice advance during the Late Weichselian glaciation could not be determined in the study. The upper continental slope is characterised by iceberg sedimentation with additional contribution from distal remnants of meltwater outflows escaping from East Greenland, sea ice rafting and pelagic settling. Mass wasting is recognised by the presence of debris flows, which are derived from the rapid and unstable build-up of large volumes of glacigenic sediment. Mass wasting events are intermittent, vary from small to large scale, and are derived from local slope regions. The mid to lower continental slope are characterised by rain out and suspension settling punctuated by intermittent sediment gravity flows. Sea ice conditions during the Late Weichselian are extended resulting in reduced ventilation of ocean surface waters and decreased exchange of CO2 between the atmosphere and ocean. Sedimentation rates are high in relation to sedimentation being focused onto the continental margin as ice advances to the inner continental shelf.
APA, Harvard, Vancouver, ISO, and other styles
6

Weinschütz, 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.

Full text
Abstract:
Orientador: Joel Carneiro de Castro
Banca: 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
APA, Harvard, Vancouver, ISO, and other styles

Books on the topic "Glacimarine"

1

Glacimarine environments. London: Geological Society, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

A, Dowdeswell J., and Scourse James D, eds. Glacimarine environments: Processes and sediments. London: Geological Society, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Dowdeswell, J. A. Glacimarine Environments: Processes and Sediments (Geological Society Special Publication). Amer Assn of Petroleum Geologists, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles

Book chapters on the topic "Glacimarine"

1

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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Catto, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Bell, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Geertsema, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Hesse, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Barrett, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Whittington, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

"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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

OCOFAIGH, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

ÓCofaigh, 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.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Glacimarine"

1

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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Glacimarine' for particular source types:
Journal articles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography