Sandeep Singh

Prof. Dr. Sandeep Singh

orcid

Research Focus & Metrics

Academic Career Length

34Years (1993-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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30 May 2005 in Earth and Planetary Science Letters
Verified
Journal Article
Closed access
MLM Leech
M Leech
SSSandeep Singh
Sandeep Singh
AJArvind Kumar Jain
Arvind Kumar Jain
SKS Klemperer
S Klemperer
RMR Manickavasagam
R Manickavasagam

1 July 2000 in Earth and Planetary Science Letters
Verified
Journal Article
Closed access
AJArvind Kumar Jain
Arvind Kumar Jain
DKDevender Kumar
Devender Kumar
SSSandeep Singh
Sandeep Singh
AKAshok Kumar
Ashok Kumar
NLNand Lal
Nand Lal



5 February 2009 in Geological Society of America Bulletin
Verified
Journal Article
Closed access
PDF file
AJA.K. Jain
A.K. Jain
NLNand Lal
Nand Lal
BSB. Sulemani
B. Sulemani
AAA.K. Awasthi
A.K. Awasthi
SSSandeep Singh
Sandeep Singh
DKDevender Kumar
Devender Kumar
Detrital-zircon fission-track (FT) ages from the Lower Cenozoic Sub-Himalayan foreland basin reflect the progressive effects of crustal thickening and exhumation on the Himalayan source rocks as a consequence of the India-Asia collision. The oldest stratum, the transgressive marine Paleocene-Eocene Subathu Formation (57–41.5 Ma) contains ca. 50 Ma detrital-zircon P1 peak, which was derived from the Indus Tsangpo Suture Zone and the Ladakh Batholith of the Asian plate. A dominant 302.4 ± 21.9 Ma peak with a few 520 Ma grains in this formation has been derived by erosion of the zircon partial-annealing zone (ZPAZ) of 240–180 °C. As the first imprint of the collision, this zone affected the Himalayan Proterozoic basement and its Tethyan sedimentary cover.

1 May 2007 in Journal of Asian Earth Sciences
Verified
Journal Article
Closed access
SSSandeep Singh
Sandeep Singh
RKRajeev Kumar
Rajeev Kumar
MBMark E. Barley
Mark E. Barley
AJArvind Kumar Jain
Arvind Kumar Jain