Sedimentary characteristics and depositional evolution of carbonate platform during the Cambrian and Ordovician in eastern Tarim Basin, NW China

Author:

Liu Jingyan,Xia Shiqiang,Zhang Junlong,He Feng,Cheng Yuhan,Zhu Yi,Chen Zhaoqin,Dong Huoxiang

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference53 articles.

1. Bao Z D, Jin Z J, Sun L D, Wang Z M, Wang Q H, Zhang Q M, Shi X Z, Li W, Wu M B, Gu Q Y, Wu X M, Zhang H W (2006). Sea-level fluctuation of the Tarim area in the early Paleozoic: respondence from geochemistry and karst. Acta Geol Sin, 80: 366–373

2. Chen Y Q, Wang X X, He H, Yi Y (2022). Evolution of uplift and depression framework of Tarim Craton in Nanhua-Cambrian. China Petrol Explor, 27: 30–46 (in Chinese)

3. Dong S L, Li Z, Xu J Q, Gao J, Guo C T (2014). Detrital zircon U-Pb geochronology and Hf isotopic compositions of Middle-Upper Ordovician sandstones from the Quruqtagh area, eastern Tarim Basin: implications for sedimentary provenance and tectonic evolution. Chin Sci Bull, 59(10): 1002–1012

4. Dunham R J (1962). Classification of Carbonate rocks according to their depositional texture. In: Ham W E, ed. Classification of Carbonate Rocks. A Symposium: AAPG Memoir: 108–121

5. Feng Z Z, Bao Z D, Wu M B, Jin Z K, Shi X Z (2006). Lithofacies palaeogeography of the Cambrian in Tarim area. J Palaeogeogra, 8: 427–439 (in Chinese)

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