A comparison of hydrothermal events and petroleum migration between Ediacaran and lower Cambrian carbonates, Central Sichuan Basin-Reference-Cited by-同舟云学术

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A comparison of hydrothermal events and petroleum migration between Ediacaran and lower Cambrian carbonates, Central Sichuan Basin

Published:2023-04 Issue: Volume:150 Page:106130
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Li Kaikai,Gong Binran,Zhang Xinghe,Jiang Hua,Fan Junjia,Tan Yineng

Funder

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference138 articles.

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2. Organic maturation and ore precipitation in Southeast Missouri;Anderson;Econ. Geol.,1991

3. Impact of geodynamics on fluid circulation and diagenesis of carbonate reservoirs in a foreland basin: example of the Upper Lacq reservoir (Aquitaine basin, SW France);Bahnan;Mar. Petrol. Geol.,2020

4. Experimental study of the interaction of mineral-forming hydrothermal solutions with oil and their joint migration;Balitsky;Petrology,2007

5. The solubility of sphalerite and galena in NaCl brines;Barrett;Econ. Geol.,1982

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1. Logging Identification Method for Reservoir Facies in Fractured-Vuggy Dolomite Reservoirs Based on AI: A Case Study of Ediacaran Dengying Formation, Sichuan Basin, China;Applied Sciences;2024-08-25

2. Characteristics and sedimentary evolution of late Ediacaran-early Cambrian microbial carbonates, chert, and phosphorite in South China;International Geology Review;2024-06-12

3. Diagenesis and pressure evolution in Ediacaran carbonate rocks in the North Slope (Penglai area) of the central Sichuan Basin (SW China);Marine and Petroleum Geology;2024-06

4. Geochemical properties, mechanism of formation, and source of solid bitumen in the Ediacaran Dengying Formation from the central to northern Sichuan Basin, China;Marine and Petroleum Geology;2024-01

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