Paleoclimate evolution and aridification mechanism of the eastern Tethys during the Callovian–Oxfordian: evidence from geochemical records of the Qiangtang Basin, Tibetan Plateau

Author:

Zeng YongyaoORCID,Gao Lei,Zhao Wenqing

Funder

National Basic Research Program of China

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference65 articles.

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2. Bai SH (1989) New recognition of marine Jurassic strata in southwestern Qinghai. Geol Rev 35(6):529–536 (in Chinese with English abstract)

3. Barskov IS, Kiyashko SI (2000) Thermal regime variations in the Jurassic marine basin of the East European Platform at the Callovian/Oxfordian boundary: Evidence from stable isotopes in belemnite rostra. Dokl Earth Sci 372:643–645

4. Bartolini A, Pittet B, Mattioli E, Hunziker JC (2003) Shallow-platform palaeoenvironmental conditions recorded in deep-shelf sediments: C and O stable isotopes in Upper Jurassic sections of southern Germany (Oxfordian-Kimmeridgian). Sediment Geol 160:107–130

5. BGMRXAR (Bureau of Geology Mineral Resources of Xizang Autonomous Region) (1993) Regional Geology of Xizang (Tibet) Autonomous Region. Geological Publishing House, Beijing, China, pp 1–450 (in Chinese with English abstract).

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