吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

张晓宝; 何海清; 陈国俊

ISSN 1000-0550 CN 62-1038/P

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吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

张晓宝, 何海清, 陈国俊

文章导航 > 沉积学报 > 1997 > 15(4): 109-114

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

引用本文:

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

Zhang Xianbao, He Haiqing, Chen Guojun. A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance[J]. Acta Sedimentologica Sinica, 1997, 15(4): 109-114.

Citation:

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

引用本文:

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

Citation:

吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

中国科学院兰州地质研究所,兰州 730000

详细信息

作者简介:
张晓宝男 38岁博士生副研究员

中图分类号: P512.2

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文章访问数: 473
HTML全文浏览量: 15
PDF下载量: 535
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A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

Lanzhou Institute of Geology,Academiasinica,Lanzhou,730000

摘要

摘要: 利用物源方向综合判识方法，通过吐哈盆地草南１井中侏罗统与物源区岩性特征以及草南１井与邻井地层厚度、岩石学特征和沉积相时空分布等方面的对比研究，认为其物源应来自于盆地南部的觉罗塔格山。这一研究成果对于完善沉积盆地物源方向判识方法，指导油气勘探部署均具有十分重要的意义.
- 物源方向 /
- 中侏罗统 /
- 草南1井 /
- 吐哈盆地
Abstract: The source direction of the Middle Jurasic of Chaonan 1 Well in Tuha Basin was comprehensivelyjudged through a comparative research on its lithologic characteristics of source areas and of its stratumthickness, and special distrilution of sedimentary facies of adjcent wells.The lithological difference of thenorth and south boundary mountains in Tuha Basin is clear, i.e, the southern Jueluotage Mt.is predormi-nated by acidic igneous rocks while the northern Bogeda Mt.by intermediate to basic rocks.The Clarkevalues of petrogenic elements, K, Ca, Mg, ferric family elements, Fe, Ni, Fe, rare earth elements, Sr, Ga,Rb, Ba of the Middle Jurassic mudstones of the Chaonan 1 Well were close to those of acidic igneousrocks.The two heavy mineral associations, rich in zircon and magnetite, respectively, basicatly represented those of acidic igneous rocks.The content of quartz in sandstones was over 20 %, the microcline andorthoclase were high while the anothesite low, and the volcanicdebris were mainly intermediate acidicones, which are closely related with acidic igneous rocks.It coued initally be concluded from the abovethat the clasts of Chaonan 1 Well were derived from the southern Jueluotage Mt.From Yue 1 Well, sour-thern to Chaonan 1 Well, to Xiaochao 1 Well, northern to Chaonan 1 Well, the thickness of sandstonesbecame thin, the size smaller, and the physical properties worse.The thickness of mudstones got thicker,the color darker, the content of sands less, the content of organic matter higher and the type of organicmatter better.Because the content of clay minerals, especially kaolinite,inceased and the mudstone thick-ened, the seal conditions were better.The above research result is of great significance in perfecting thejudgement method of source direction of sedimentary basins, predicting the distribution of the most fa-vorable reservoir bodies and source-reservoir-caprock associations and guiding the exploration of oils andgases.
- source direction /
- Middle Jurassic /
- Chaonan 1 Well /
- Tuha Basin

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参考文献(1)

[1]	(1) 袁明生,王武和,曾晓明.吐哈盆地成油条件及勘探方向.吐哈盆地石油地质研究论文集 (王昌桂、路锡良主编),北京: 石油工业出版社, 1995, 6～15. (2) 陈煦.台北凹陷中侏罗统物源区母岩性质及物源分析.吐哈盆地石油地质研究论文集(王昌桂,路锡良主编),北京: 石油工业出版社, 1995, 98～101.

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吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

中国科学院兰州地质研究所,兰州 730000

作者简介:
张晓宝男 38岁博士生副研究员

收稿日期: 1996-06-12
刊出日期: 1997-12-10

中图分类号: P512.2

关键词:

物源方向 /

中侏罗统 /

草南1井 /

吐哈盆地

摘要: 利用物源方向综合判识方法，通过吐哈盆地草南１井中侏罗统与物源区岩性特征以及草南１井与邻井地层厚度、岩石学特征和沉积相时空分布等方面的对比研究，认为其物源应来自于盆地南部的觉罗塔格山。这一研究成果对于完善沉积盆地物源方向判识方法，指导油气勘探部署均具有十分重要的意义.

English Abstract

A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

Lanzhou Institute of Geology,Academiasinica,Lanzhou,730000

Received Date: 1996-06-12
Publish Date: 1997-12-10

Keywords:

Abstract: The source direction of the Middle Jurasic of Chaonan 1 Well in Tuha Basin was comprehensivelyjudged through a comparative research on its lithologic characteristics of source areas and of its stratumthickness, and special distrilution of sedimentary facies of adjcent wells.The lithological difference of thenorth and south boundary mountains in Tuha Basin is clear, i.e, the southern Jueluotage Mt.is predormi-nated by acidic igneous rocks while the northern Bogeda Mt.by intermediate to basic rocks.The Clarkevalues of petrogenic elements, K, Ca, Mg, ferric family elements, Fe, Ni, Fe, rare earth elements, Sr, Ga,Rb, Ba of the Middle Jurassic mudstones of the Chaonan 1 Well were close to those of acidic igneousrocks.The two heavy mineral associations, rich in zircon and magnetite, respectively, basicatly represented those of acidic igneous rocks.The content of quartz in sandstones was over 20 %, the microcline andorthoclase were high while the anothesite low, and the volcanicdebris were mainly intermediate acidicones, which are closely related with acidic igneous rocks.It coued initally be concluded from the abovethat the clasts of Chaonan 1 Well were derived from the southern Jueluotage Mt.From Yue 1 Well, sour-thern to Chaonan 1 Well, to Xiaochao 1 Well, northern to Chaonan 1 Well, the thickness of sandstonesbecame thin, the size smaller, and the physical properties worse.The thickness of mudstones got thicker,the color darker, the content of sands less, the content of organic matter higher and the type of organicmatter better.Because the content of clay minerals, especially kaolinite,inceased and the mudstone thick-ened, the seal conditions were better.The above research result is of great significance in perfecting thejudgement method of source direction of sedimentary basins, predicting the distribution of the most fa-vorable reservoir bodies and source-reservoir-caprock associations and guiding the exploration of oils andgases.

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

引用本文:

张晓宝, 何海清, 陈国俊. 吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义[J]. 沉积学报, 1997, 15(4): 109-114.

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吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

作者简介:
张晓宝男 38岁博士生副研究员

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A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

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目录

吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

中国科学院兰州地质研究所,兰州 730000

作者简介:
张晓宝男 38岁博士生副研究员

English Abstract

A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

Lanzhou Institute of Geology,Academiasinica,Lanzhou,730000

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吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

作者简介: 张晓宝 男 38岁 博士生 副研究员

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A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

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出版历程

目录

吐哈盆地草南1井中侏罗统物源方向综合判识及其研究意义

中国科学院兰州地质研究所,兰州 730000

作者简介: 张晓宝 男 38岁 博士生 副研究员

English Abstract

A Comprehensive Judgement of the Source Direction of the Middle Jurassic of Chaonan 1 Well in the Tuha Basin and Its Research Significiance

Lanzhou Institute of Geology,Academiasinica,Lanzhou,730000

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
张晓宝男 38岁博士生副研究员

作者简介:
张晓宝男 38岁博士生副研究员