四川旺苍志留系鲕粒灰岩特征及地质意义

秦松; 张涛; 苏文博; 王巍; 马超

doi:10.3799/dqkx.2011.005

Volume 36 Issue 1

Jan. 2011

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QIN Song, ZHANG Tao, SU Wen-bo, WANG Wei, MA Chao, 2011. Characteristics and Implications of the Oolitic Limestones from the Silurian Succession in Wangcang, Sichuan, South China. Earth Science, 36(1): 43-52. doi: 10.3799/dqkx.2011.005

Citation:

QIN Song, ZHANG Tao, SU Wen-bo, WANG Wei, MA Chao, 2011. Characteristics and Implications of the Oolitic Limestones from the Silurian Succession in Wangcang, Sichuan, South China. Earth Science, 36(1): 43-52. doi: 10.3799/dqkx.2011.005

Citation:

QIN Song, ZHANG Tao, SU Wen-bo, WANG Wei, MA Chao, 2011. Characteristics and Implications of the Oolitic Limestones from the Silurian Succession in Wangcang, Sichuan, South China. Earth Science, 36(1): 43-52. doi: 10.3799/dqkx.2011.005

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Characteristics and Implications of the Oolitic Limestones from the Silurian Succession in Wangcang, Sichuan, South China

doi: 10.3799/dqkx.2011.005

QIN Song^1
,,
ZHANG Tao²,
SU Wen-bo^{1
,
,},
WANG Wei¹,
MA Chao¹

1.
School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Regional Investigation Team in Geological Prospecting Bureau of Sichuan, Shuangliu 610213, China

Received Date: 2010-05-31
Publish Date: 2011-01-01

Abstract

Abstract

Oolitic limestone has been recognized for the first time in the Early Silurian (Telychian) Nanjiang Formation from Wangcang, NW Sichuan. Facies analyses show that this oolitic-bearing succession developed in a ramp environment. With the thickness less than 10 cm in general and interbedded in the ramp succession, it can be determined that the oolitic layers were moved by episodic currents probably from a large oolitic beach near Wangcang, NW Sichuan, Upper Yangtze platform. Under the microscope, the categories of the oolites are monotonous, and somewhat compressed and deformed, with close contacts and serrated appearances. It also indicates that the oolites should be well-sorted and transported under the high-energy environment, and then be compacted during the following diagenetic stage. The oxygen and carbon isotope analyses of the oolites indicate that the paleotemperature is 25-31 ℃, suggesting tropical to subtropical climates of the mediate to low latitude during the Early Silurian (Telychian) in the Upper Yangtze region. Besides the study of the paleoclimate and paleogeography, as the high-quality reservoir rock, the discovery of the Early Silurian oolitic beds and the possible related oolitic beach nearby is helpful for the oil-gas exploration in NW Sichuan.
- oolitic limestone,
- paleoclimate,
- Silurian,
- sedimentation,
- Upper Yangtze platform

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References(74)

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Characteristics and Implications of the Oolitic Limestones from the Silurian Succession in Wangcang, Sichuan, South China

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