Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China

The distribution of solid bitumen in the Devonian carbonate reservoir from well Desheng 1, Guizhong Depression, was investigated by optical microscope and hydrocarbon inclusions analysis. Vb and chemical structure indexes measured by bitumen reflectance, laser Raman microprobe (LRM), and Fourier tra...

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Main Authors: Yuguang Hou, Yaqi Liang, Sheng He, Yukun Liu, Zhiwei Fan, Yingrui Song
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2017/4580416
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author Yuguang Hou
Yaqi Liang
Sheng He
Yukun Liu
Zhiwei Fan
Yingrui Song
author_facet Yuguang Hou
Yaqi Liang
Sheng He
Yukun Liu
Zhiwei Fan
Yingrui Song
author_sort Yuguang Hou
collection DOAJ
description The distribution of solid bitumen in the Devonian carbonate reservoir from well Desheng 1, Guizhong Depression, was investigated by optical microscope and hydrocarbon inclusions analysis. Vb and chemical structure indexes measured by bitumen reflectance, laser Raman microprobe (LRM), and Fourier transform infrared spectroscopy (FTIR) were carried out to determine the thermal maturity of solid bitumen. Based on the solid bitumen thermal maturity, the burial and thermal maturity history of Devonian carbonate reservoir were reconstructed by basin modeling. The results indicate that the fractures and fracture-related dissolution pores are the main storage space for the solid bitumen. The equivalent vitrinite reflectance of solid bitumen ranges from 3.42% to 4.43% converted by Vb (%) and LRM. The infrared spectroscopy analysis suggests that there are no aliphatic chains detected in the solid bitumen which is rich in aromatics C=C chains (1431–1440 cm−1). The results of Vb (%), LRM, and FTIR analysis demonstrate that the solid bitumen has experienced high temperature and evolved to the residual carbonaceous stage. The thermal evolution of Devonian reservoirs had experienced four stages. The Devonian reservoirs reached the highest reservoir temperature 210–260°C during the second rapid burial-warming stage, which is the main period for the solid bitumen formation.
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institution Kabale University
issn 1468-8115
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language English
publishDate 2017-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-263384b59a2d40e691bd3455e5c85e872025-02-03T05:43:36ZengWileyGeofluids1468-81151468-81232017-01-01201710.1155/2017/45804164580416Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South ChinaYuguang Hou0Yaqi Liang1Sheng He2Yukun Liu3Zhiwei Fan4Yingrui Song5China University of Geosciences Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan 430074, ChinaChina University of Geosciences Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan 430074, ChinaChina University of Geosciences Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan 430074, ChinaChina University of Geosciences Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan 430074, ChinaPetroleum Exploration Branch Company, Sinopec, Chengdu 610041, ChinaChina University of Geosciences Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan 430074, ChinaThe distribution of solid bitumen in the Devonian carbonate reservoir from well Desheng 1, Guizhong Depression, was investigated by optical microscope and hydrocarbon inclusions analysis. Vb and chemical structure indexes measured by bitumen reflectance, laser Raman microprobe (LRM), and Fourier transform infrared spectroscopy (FTIR) were carried out to determine the thermal maturity of solid bitumen. Based on the solid bitumen thermal maturity, the burial and thermal maturity history of Devonian carbonate reservoir were reconstructed by basin modeling. The results indicate that the fractures and fracture-related dissolution pores are the main storage space for the solid bitumen. The equivalent vitrinite reflectance of solid bitumen ranges from 3.42% to 4.43% converted by Vb (%) and LRM. The infrared spectroscopy analysis suggests that there are no aliphatic chains detected in the solid bitumen which is rich in aromatics C=C chains (1431–1440 cm−1). The results of Vb (%), LRM, and FTIR analysis demonstrate that the solid bitumen has experienced high temperature and evolved to the residual carbonaceous stage. The thermal evolution of Devonian reservoirs had experienced four stages. The Devonian reservoirs reached the highest reservoir temperature 210–260°C during the second rapid burial-warming stage, which is the main period for the solid bitumen formation.http://dx.doi.org/10.1155/2017/4580416
spellingShingle Yuguang Hou
Yaqi Liang
Sheng He
Yukun Liu
Zhiwei Fan
Yingrui Song
Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
Geofluids
title Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
title_full Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
title_fullStr Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
title_full_unstemmed Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
title_short Distribution and Thermal Maturity of Devonian Carbonate Reservoir Solid Bitumen in Desheng Area of Guizhong Depression, South China
title_sort distribution and thermal maturity of devonian carbonate reservoir solid bitumen in desheng area of guizhong depression south china
url http://dx.doi.org/10.1155/2017/4580416
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