Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea

The main factors of the developmental environment of marine source rocks in continental margin basins have their specificality. This realization, in return, has led to the recognition that the developmental environment and pattern of marine source rocks, especially for the source rocks in continenta...

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Main Authors: Wenhao Li, Zhihuan Zhang, Weiming Wang, Shuangfang Lu, Youchuan Li, Ning Fu
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2014/240415
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author Wenhao Li
Zhihuan Zhang
Weiming Wang
Shuangfang Lu
Youchuan Li
Ning Fu
author_facet Wenhao Li
Zhihuan Zhang
Weiming Wang
Shuangfang Lu
Youchuan Li
Ning Fu
author_sort Wenhao Li
collection DOAJ
description The main factors of the developmental environment of marine source rocks in continental margin basins have their specificality. This realization, in return, has led to the recognition that the developmental environment and pattern of marine source rocks, especially for the source rocks in continental margin basins, are still controversial or poorly understood. Through the analysis of the trace elements and maceral data, the developmental environment of Miocene marine source rocks in the Qiongdongnan Basin is reconstructed, and the developmental patterns of the Miocene marine source rocks are established. This paper attempts to reveal the hydrocarbon potential of the Miocene marine source rocks in different environment and speculate the quality of source rocks in bathyal region of the continental slope without exploratory well. Our results highlight the palaeoenvironment and its control on the formation of Miocene marine source rocks in the Qiongdongnan Basin of the northern South China Sea and speculate the hydrocarbon potential of the source rocks in the bathyal region. This study provides a window for better understanding the main factors influencing the marine source rocks in the continental margin basins, including productivity, preservation conditions, and the input of terrestrial organic matter.
format Article
id doaj-art-f816c64dfdb942e8add0174b77e6be29
institution Kabale University
issn 2356-6140
1537-744X
language English
publishDate 2014-01-01
publisher Wiley
record_format Article
series The Scientific World Journal
spelling doaj-art-f816c64dfdb942e8add0174b77e6be292025-02-03T01:27:48ZengWileyThe Scientific World Journal2356-61401537-744X2014-01-01201410.1155/2014/240415240415Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China SeaWenhao Li0Zhihuan Zhang1Weiming Wang2Shuangfang Lu3Youchuan Li4Ning Fu5Research Institute of Unconventional Petroleum and Renewable Energy, China University of Petroleum, Qingdao 266580, ChinaState Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, ChinaResearch Institute of Unconventional Petroleum and Renewable Energy, China University of Petroleum, Qingdao 266580, ChinaResearch Institute of Unconventional Petroleum and Renewable Energy, China University of Petroleum, Qingdao 266580, ChinaChina National Offshore Oil Corporation, Beijing 100027, ChinaChina National Offshore Oil Corporation, Beijing 100027, ChinaThe main factors of the developmental environment of marine source rocks in continental margin basins have their specificality. This realization, in return, has led to the recognition that the developmental environment and pattern of marine source rocks, especially for the source rocks in continental margin basins, are still controversial or poorly understood. Through the analysis of the trace elements and maceral data, the developmental environment of Miocene marine source rocks in the Qiongdongnan Basin is reconstructed, and the developmental patterns of the Miocene marine source rocks are established. This paper attempts to reveal the hydrocarbon potential of the Miocene marine source rocks in different environment and speculate the quality of source rocks in bathyal region of the continental slope without exploratory well. Our results highlight the palaeoenvironment and its control on the formation of Miocene marine source rocks in the Qiongdongnan Basin of the northern South China Sea and speculate the hydrocarbon potential of the source rocks in the bathyal region. This study provides a window for better understanding the main factors influencing the marine source rocks in the continental margin basins, including productivity, preservation conditions, and the input of terrestrial organic matter.http://dx.doi.org/10.1155/2014/240415
spellingShingle Wenhao Li
Zhihuan Zhang
Weiming Wang
Shuangfang Lu
Youchuan Li
Ning Fu
Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
The Scientific World Journal
title Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
title_full Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
title_fullStr Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
title_full_unstemmed Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
title_short Palaeoenvironment and Its Control on the Formation of Miocene Marine Source Rocks in the Qiongdongnan Basin, Northern South China Sea
title_sort palaeoenvironment and its control on the formation of miocene marine source rocks in the qiongdongnan basin northern south china sea
url http://dx.doi.org/10.1155/2014/240415
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