Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon
The data is from the attachment of the paper. Data sets include
S1 geological and sedimentary setting
S3 Zircon U-Pb dating and depositional age constraints
S3 TABLES， including; U-Pb isotopic analysis of detrital zircons from Liuqu, Qiuwu and Dazuqu Formations, Major elements data for minerals comprising the tuffite by electron probe microanalysis, CLAMP scores describing woody dicot leaf form within the Liuqu, Qiuwu, Namling and India paleofloras, Climatic parameters predicted by CLAMP and their associated statistical uncertainties, Paleoelevation estimated by CLAMP,
S4 diagram, includingRepresentative leaf fossils from the Liuqu Formation, Gongjiongla and Za localities, Mean age diagram for a tuffite, Zircon U-Pb age probability density diagram, Diorite clasts from Liuqu conglomerate and zircon age diagram, Representative leaf fossils from the Qiuwu Formation, Field photographs, Annual average moist enthalpy at mean sea level
Ding, L. (2020). Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon. National Tibetan Plateau Data Center, DOI: 10.11888/Geo.tpdc.270351. CSTR: 18406.11.Geo.tpdc.270351. (Download the reference： RIS | Bibtex )Related Literatures:
1. Ding, L., Spicer, R.A., Yang, J., Xu, Q., Cai, F.L., Li, S., Lai, Q.Z., Wang, H.Q., Spicer, T.E.V., Yue, Y.H., Shukla, A., Srivastava, G., Khan, M.A., Bera, S., and Mehrotra, R. 2017. Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon. Geology, 45:215-218.( View Details | Download | Bibtex)
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