This data set is from the paper: 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 origin and implications for the South Asian monsoon. Geography, 45:215-218. This achievement is part of a series of research results of paleoaltitude carried out by Ding Lin' team. We reconstruct the rise of a segment of the southern flank of the Himalaya-Tibet orogen, to the south of the Lhasa terrane, using a paleoaltimeter based on paleoenthalpy encoded in fossil leaves from two new assemblages in southern Tibet (Liuqu and Qiabulin) and four previously known floras from the Himalaya foreland basin. U-Pb dating of zircons constrains the Liuqu flora to the latest Paleocene (ca. 56 Ma) and the Qiabulin flora to the earliest Miocene (21–19 Ma). The proto-Himalaya grew slowly against a high (~4 km) proto–Tibetan Plateau from ~1 km in the late Paleocene to ~2.3 km at the beginning of the Miocene, and achieved at least ~5.5 km by ca. 15 Ma. Contrasting precipitation patterns between the Himalaya-Tibet edifice and the Himalaya foreland basin for the past ~56 m.y. show progressive drying across southern Tibet, seemingly linked to the uplift of the Himalaya orogen.

File naming and required software

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

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Cite as:

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)

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.

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