桩海地区下古生界潜山内新一类储层：硅化岩储层的发现及特征

于正军; 许淑梅; 王金铎; 于建国; 韩文功; 李三忠; 马云

doi:10.3799/dqkx.2010.009

Volume 35 Issue 1

Jan. 2010

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Article Navigation > Earth Science > 2010 > 35(1): 87-96

YU Zheng-jun, XU Shu-mei, WANG Jin-duo, YU Jian-guo, HAN Wengong, LI San-zhong, MA Yun, 2010. A New Type of Reservoir of Paleozoic Buried Hill in Zhuanghai Area: Discovery and Characteristics of Silicified Rock. Earth Science, 35(1): 87-96. doi: 10.3799/dqkx.2010.009

Citation:

YU Zheng-jun, XU Shu-mei, WANG Jin-duo, YU Jian-guo, HAN Wengong, LI San-zhong, MA Yun, 2010. A New Type of Reservoir of Paleozoic Buried Hill in Zhuanghai Area: Discovery and Characteristics of Silicified Rock. Earth Science, 35(1): 87-96. doi: 10.3799/dqkx.2010.009

Citation:

YU Zheng-jun, XU Shu-mei, WANG Jin-duo, YU Jian-guo, HAN Wengong, LI San-zhong, MA Yun, 2010. A New Type of Reservoir of Paleozoic Buried Hill in Zhuanghai Area: Discovery and Characteristics of Silicified Rock. Earth Science, 35(1): 87-96. doi: 10.3799/dqkx.2010.009

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A New Type of Reservoir of Paleozoic Buried Hill in Zhuanghai Area: Discovery and Characteristics of Silicified Rock

doi: 10.3799/dqkx.2010.009

YU Zheng-jun^{1, 2, 3
,},
XU Shu-mei^{4, 5
,},
WANG Jin-duo²,
YU Jian-guo²,
HAN Wengong⁴,
LI San-zhong^{4, 5},
MA Yun⁴

1.
Key Laboratory of Marine Geology & Environment, Institute of Oceaology, Chinese Academy of Sciences, Qingdao 266071, China
2.
Geophysical Research Institute, Shengli Oilfield, SINOPEC, Dongying 257022, China
3.
Graduate University, Chinese Academy of Sciences, Beijing 100083, China
4.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
5.
Key Lab of Marine Geosciences and Exploration, Ministry of Education, Qingdao 266100, China

Received Date: 2009-05-10
Publish Date: 2010-01-01

Abstract

Abstract

Based on the core description, microanalysis and processing of the logging data including AC, GR and DEN, a new type of silicalite reservoirs in Paleozoic buried hill in Zhuanghai area is found whose rock-electric properties are very different from those of protogenesis silicalites. Silicalite reservoirs are called silicified rock here and their characteristics are generalized. The structure of primary rock of silicified rock is clear and the idiomorphic degree of quartz crystal is high. Paragentic hydrothermal mineral assemblage of fluorite, barite, pyrite, ferrocalcite and quartz with secondary characteristic are common in silicified rock layer and the secondary corrosion of these paragentic hydrothermal minerals is significant. The pore of silicified layer is very developed including not only large solution cavities among breccias and secondary pores by dissolution of the Paragentic hydrothermal minerals, but also the micro-pores among the idiomorphic quartz crystal druse. The P-wave velocity and the density of silicified rock are much lower than that of the carbonate and the distribution of silicified rock in buried hill is featured with the "cross-layer" characteristic. By comparing with the characteristic of the protogenesis silicalite in Paleozoic buried hill, it is believed that the silicified rock is secondary genesis which resulted from deep buried modification. The secondary silicified rock is a new type of reservoir of Paleozoic buried hill in Zhuanghai area. The discovery of this new kind of reservoirs is not only of value to the high exploration basin, but also of scientific significance to the advance of silicate research.
- (secondary) silicified rock,
- reservoir,
- Paleozoic,
- petrology,
- Zhuanghai area

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References(70)

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A New Type of Reservoir of Paleozoic Buried Hill in Zhuanghai Area: Discovery and Characteristics of Silicified Rock

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