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Sidney R. Hemming

Researcher at Lamont–Doherty Earth Observatory

Publications -  232
Citations -  12685

Sidney R. Hemming is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Glacial period & Ice sheet. The author has an hindex of 49, co-authored 205 publications receiving 11146 citations. Previous affiliations of Sidney R. Hemming include Stony Brook University & Columbia University.

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Clay separation and x-ray diffraction for refined k/ar dating of fault motion on the creeping central section of the san andreas fault

TL;DR: In this article , a York regression between age and detrital illite abundance was used to estimate the age at which there was 0% detritality and 100% authigenic illite.
Journal Article

IODP Expedition 361 – Southern African Climates and Agulhas LGM Density Profile

TL;DR: IODP Expedition 361 as mentioned in this paper explored the Agulhas Current during the Plio-Pleistocene in association with transient to long-term changes of highlatitude climates, tropical heat budgets, and the monsoon system.
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Marine sediment provenance evidence for the extent of the laurentide ice sheet during the last glacial cycle

TL;DR: In this article , the authors review the evidence for armadas of icebergs from Hudson Strait during Heinrich events, especially H1, H2, H4 and H5, and review the record of continuous down core measurements of ice rafted hornblende provenance, that provides evidence that the southeastern Laurentide ice sheet reached latitudes required to tap Grenvillian (ca 1.0-1.2 Ga) and Appalachian (ca 0.3-0.4 Ga) geological terrains immediately after H3 and retreated from that around H1.
Posted ContentDOI

Pliocene-Pleistocene evolution of the Agulhas leakage to the Atlantic Ocean

TL;DR: Hall et al. as discussed by the authors investigated the longer-term evolution of Agulhas leakage during the Pliocene and Pleistocene (the last 5.3 Ma) and found that the Agulha leakage was reinvigorated during deglaciations and was, in turn, potentially important for the development of interglacial warmth.