海相烃源岩的正反演对比分析

解习农; 殷鸿福; 谢树成

Volume 32 Issue 6

Jun. 2007

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XIE Xi-nong, YIN Hong-fu, XIE Shu-cheng, 2007. Comparison on Forward and Inverse Analysis Methods of Marine Hydrocarbon Source Rocks. Earth Science, 32(6): 861-867.

Citation:

XIE Xi-nong, YIN Hong-fu, XIE Shu-cheng, 2007. Comparison on Forward and Inverse Analysis Methods of Marine Hydrocarbon Source Rocks. Earth Science, 32(6): 861-867.

XIE Xi-nong, YIN Hong-fu, XIE Shu-cheng, 2007. Comparison on Forward and Inverse Analysis Methods of Marine Hydrocarbon Source Rocks. Earth Science, 32(6): 861-867.

Citation:

XIE Xi-nong, YIN Hong-fu, XIE Shu-cheng, 2007. Comparison on Forward and Inverse Analysis Methods of Marine Hydrocarbon Source Rocks. Earth Science, 32(6): 861-867.

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Comparison on Forward and Inverse Analysis Methods of Marine Hydrocarbon Source Rocks

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2007-08-12
Publish Date: 2007-11-25

Abstract

Abstract

An effective evaluation system of high-quality marine source rocks plays an important role in hydrocarbon exploration and exploitation of marine strata. Remnant organic matter preserved in a sedimentary basin underwent two evolutionary stages from organic matter to source rocks, i.e. the formation of deposited organic matter and the formation of source rocks transferring from deposited organic matter to remnant organic matter. The latter includes the immature stage during which the deposited organic matter experienced biogeochemical processes to become burial organic matter, and the mature and the post-mature stages during which the burial organic matter underwent geothermal processes to become remnant organic matter and subsequently to be weathered. The inverse analysis of source rocks is defined as a method and technique to estimate the amount of burial organic matter and original potential of hydrocarbon generation of source rocks based on the analysis of remnant or weathered organic matter. The forward analysis of source rocks is defined as a method to estimate the amount of depositional organic matter or burial organic matter, and ulteriorly to estimate their original potential of hydrocarbon generation of source rocks by using the information of sedimentary environments, features of living biomass and physical chemistry in water medium through the geobiological analysis of geoecology, geomicrobiology, molecular geobiology and biogeochemistry. Quality and quantity of depositional organic matter can be calculated according to the productivity and preservation environments. Comparison between the forward and the inverse analysis can be validated and complemented by each other, which would reveal the features of source rocks and provide an effective method for the prediction and evaluation of good-quality marine source rocks.
- marine source rocks,
- depositional organic matter,
- burial organic matter,
- remnant organic matter,
- evaluation system

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References(46)

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