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Mineralogical and isotopic data provide clues to climate change during the late Quaternary - a case study from Tso Moriri Lake, NW Himalaya (India)

Authors
/persons/resource/mishra

Mishra,  Praveen Kumar
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Prasad,  Sushma
External Organizations;

/persons/resource/anoop

Anoop,  A.
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Menzel,  P.
External Organizations;

Jehangir,  A.
External Organizations;

/persons/resource/birgit

Plessen,  B.
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/rudolf

Naumann,  R.
4.2 Inorganic and Isotope Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Gaye,  Birgit
External Organizations;

Yousuf,  Abdul
External Organizations;

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Citation

Mishra, P. K., Prasad, S., Anoop, A., Menzel, P., Jehangir, A., Plessen, B., Naumann, R., Gaye, B., Yousuf, A. (2014): Mineralogical and isotopic data provide clues to climate change during the late Quaternary - a case study from Tso Moriri Lake, NW Himalaya (India), (Geophysical Research Abstracts, Vol. 16, EGU2014-10525, 2014), General Assembly European Geosciences Union (Vienna, Austria 2014).


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_391741
Abstract
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