塔里木盆地塔中—顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征

doi:10.13278/j.cnki.jjuese.20170307

Abstract

Abstract: The Ordovician carbonate shoals in Tazhong and Shuntuoguole area have good prospects for hydrocarbon resources. The definition and classification of carbonate shoals are clarified in this paper. Based on the analysis of thin sections, the carbonate shoals of Lianglitage Formation could be classified into three types:intra-clastic shoal, oolitic shoal and bioclastic shoal, containing mainly intra-clast, bio-clast, and ooid. Most of the carbonate shoals are bright crystal cement, reflecting a high-energy hydrodynamic environment. Different grains are often associated with each other because of migration. The compound ooid developed in low energy environment and the algae grain from middle-high energy environment are also identified. Algae grains are developed usually together with intra-clast and bio-clast, although not abundant, and formed in a middle-high energy tidal flat environment and gentle slope of carbonate platform. The cementation type, separation and grinding are affected by the energy of sedimentary environment and hydrodynamic conditions. Through the comparison analysis of connecting wells, Lianglitage Formation could be subdivided into three third-order sequences. The stacking pattern of carbonate shoals in transgressive system tract is thin-layer cake retrograde deposit, while in high system tract that is thick-layer cake deposit. At last, the sedimentary model of carbonate shoals in this area is built through combining their distribution characteristics.

Key words: Tarim basin, Ordovician, carbonate shoals, sedimentary characteristics, sedimentary model, Lianglitage Formation

CLC Number:

TE122

Yan Wei, Zhang Guangxue, Fan Tailiang, Xia Bin, Gao Zhiqian, Zhang Li, Yang Zhen, Qiang Kunsheng. Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin[J].Journal of Jilin University(Earth Science Edition), 2019, 49(3): 621-636.

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Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin

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