TY - JOUR
T1 - Arabian Sea Monsoon
T2 - deep sea drilling in the Arabian Sea: constraining tectonic-monsoon interactions in South Asia
AU - Pandey, Dhananjai K.
AU - Clift, Peter D.
AU - Kulhanek, Denise K.
AU - Andò, Sergio
AU - Bendle, James A. P.
AU - Bratenkov, Sophia
AU - Griffith, Elizabeth M.
AU - Gurumurthy, Gundiga P.
AU - Hahn, Annette
AU - Iwai, Masao
AU - Khim, Boo-Keun
AU - Kumar, Anil
AU - Kumar, A. Ganesh
AU - Liddy, Hannah M.
AU - Lu, Huayu
AU - Lyle, Mitchell W.
AU - Mishra, Ravi
AU - Radhakrishna, Tallavajhala
AU - Routledge, Claire M.
AU - Saraswat, Rajeev
AU - Saxena, Rakesh
AU - Scardia, Giancarlo
AU - Sharma, Girish K.
AU - Singh, Arun D.
AU - Steinke, Stephan
AU - Suzuki, Kenta
AU - Tauxe, Lisa
AU - Tiwari, Manish
AU - Xu, Zhaokai
AU - Yu, Zhaojie
N1 - Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.
PY - 2015/3/31
Y1 - 2015/3/31
N2 - The Arabian Sea in the northern Indian Ocean pre-serves regional sedimentary records of rifting, tectonic subsidence, and paleoceanographic history, and also provides archives of long-term erosion of the Himalaya since the start of collision between India and Eurasia. Investigations reveal that drilling in this region can provide erosion records through analyses of the sediment cores, along with providing age control for the regional seismic stratigraphy. It is only by quantifying the volume of sediment deposited in the fan that researchers can mass balance the volume of bedrock eroded from the mountains, constrained by thermochronology, with the volume of eroded rock deposited in the offshore and in the foreland basin.
AB - The Arabian Sea in the northern Indian Ocean pre-serves regional sedimentary records of rifting, tectonic subsidence, and paleoceanographic history, and also provides archives of long-term erosion of the Himalaya since the start of collision between India and Eurasia. Investigations reveal that drilling in this region can provide erosion records through analyses of the sediment cores, along with providing age control for the regional seismic stratigraphy. It is only by quantifying the volume of sediment deposited in the fan that researchers can mass balance the volume of bedrock eroded from the mountains, constrained by thermochronology, with the volume of eroded rock deposited in the offshore and in the foreland basin.
UR - http://www.scopus.com/inward/record.url?scp=84938904443&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:84938904443
SP - 6
EP - 46
JO - Integrated Ocean Drilling Program: Preliminary Reports
JF - Integrated Ocean Drilling Program: Preliminary Reports
SN - 1932-9423
IS - 355
ER -