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Fulong Cai

Researcher at Chinese Academy of Sciences

Publications -  61
Citations -  2704

Fulong Cai is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Terrane. The author has an hindex of 20, co-authored 47 publications receiving 1799 citations. Previous affiliations of Fulong Cai include University of Arizona & Center for Excellence in Education.

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The Andean-type Gangdese Mountains: Paleoelevation record from the Paleocene-Eocene Linzhou Basin

TL;DR: In this article, the authors presented new oxygen and carbon isotopic compositions from well dated Tertiary paleosols, lacustrine calcareous carbonates, and marls from the Nianbo and upper Pana Formations of the Linzizong Group in the Linzhou (Penbo) Basin.
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Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon

TL;DR: The authors reconstructs 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 foreland basin.
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Provenance analysis of the Mesozoic Hoh-Xil-Songpan-Ganzi turbidites in northern Tibet: Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean

TL;DR: Zircon age data indicate that the Middle-Upper Triassic marine gravity-flow deposits of the Hoh-Xil-Songpan-Ganzi complex were shed from the North and South China blocks, and Middle-Late Triassic ultrahigh-pressure Qinling-Dabie orogenic belt, as well as the Kunlun and Qiangtang terranes as mentioned in this paper.
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Provenance analysis of upper Cretaceous strata in the Tethys Himalaya, southern Tibet: Implications for timing of India-Asia collision

TL;DR: In this article, in-situ detrital zircon U-Pb ages and Lu-Hf isotopic analyses, whole rock Nd-isotopes, and Cr-spinel electronic microprobe data from upper Cretaceous clastic sedimentary rocks of the Tethys Himalaya near Gyangze, southern Tibet.
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Paleogene high elevations in the Qiangtang Terrane, central Tibetan Plateau

TL;DR: In this paper, the authors present stable isotope results of fluvial/lacustrine carbonate cement, pedogenic carbonate and marl from the Kangtuo and Suonahu formations deposited between ∼51 and ∼28 Ma in the Heihuling-Bamaoqiongzong area of the northern Qiangtang terrane.