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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第41卷

期数:

2019年第03期

页码:

281-296

栏目:

基础地质与矿产地质

出版日期:

2019-05-15

文章信息/Info

Title:

Provenance Analysis of Yanghugou Formation in the Western Margin of Ordos Basin, China

文章编号:

1672-6561(2019)03-0281-16

作者:

王子腾¹; 王康乐²; 王峰^1*; 孔磊²; 田景春¹; 付勋勋²

(1.成都理工大学 油气藏地质及开发工程国家重点实验室,四川 成都 610059; 2.中国石油长庆油田分公司勘探开发研究院,陕西 西安 710018)

Author(s):

WANG Zi-teng¹;  WANG Kang-le²;  WANG Feng^1*;  KONG Lei²;  TIAN Jing-chun¹;  FU Xun-xun²

(1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi’an 710018, Shaanxi, China)

关键词:

物源区;  羊虎沟组;  母岩;  轻、重矿物组合;  Dickinson三角图解;  稀土元素;  天然气;  鄂尔多斯盆地

Keywords:

provenance;  Yanghugou Formation;  parent rock;  light and heavy mineral combination;  Dickinson triangle diagram;  REE;  natural gas;  Ordos Basin

分类号:

P618.130.2

DOI:

-

文献标志码:

A

摘要:

鄂尔多斯盆地西缘羊虎沟组物源特征对天然气勘探尤为重要。通过砂岩的碎屑组分、岩屑组分、重矿物组合以及石英阴极发光等研究,认为研究区羊虎沟组受到北部、西南部、南部物源控制,各个方位物源在研究区中部吴忠—马家滩地区汇合。通过砂岩轻、重矿物组合和碎屑组分的Dickinson三角图解,以及泥岩的稀土元素特征等分析,认为研究区羊虎沟组源岩以大陆上地壳岩石为主。研究区北部砂岩物源区为再旋回造山带物源区,泥岩球粒陨石标准化稀土元素配分模式与阿拉善古陆浅变质岩相似,具有亲缘性; 西南部及南部砂岩物源区为稳定陆块区和再旋回造山带物源区,泥岩球粒陨石标准化稀土元素配分模式与祁连—北秦岭造山带中浅变质岩相似。综上所述,研究区北部母岩主要为阿拉善古陆的浅变质岩夹少许火山岩,西南部及南部母岩主要为祁连—北秦岭造山带的中浅变质岩,其次为碳酸盐岩和火山岩。

Abstract:

The provenance characteristics of Yanghugou Formation in the western margin of Ordos Basin is particularly important for natural gas exploration. Through the studies on clastic components, lithic components, heavy mineral combination and quartz cathodoluminescence(CL)of sandstones, it is believed that Yanghugou Formation is controlled by the provenances in the north, southwest and south of the study area, which meet at Wuzhong-Majiatan area in the middle of the study area. Through the analysis on light and heavy mineral combination, Dickinson triangle diagram of debris components of sandstones, and rare earth element(REE)characteristics of mudstones, it is believed that the source rocks of Yanghugou Formation in the study area are dominated by continental crust rocks. The north sandstone provenance is a recyclic orogenic belt, the chondrite-normalized REE pattern of mudstone is similar to that of Alashan paleocontinental metamorphic rock; the southwest and south provenances are stable land masses and recyclic orogenic belts, the chondrite-normalized REE pattern of mudstone is similar to that of the shallow metamorphic rocks in Qilian-North Qinling orogenic belt. In conclusion, the parent rock in the north of the study area is mainly a shallow metamorphic rock with a small volcanic rock in Alashan paleocontinent, and the parent rocks in the southwest and south are mainly the medium-shallow metamorphic rocks in Qilian-North Qinling orogenic belt, followed by carbonate and volcanic rocks.

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相似文献/References:

备注/Memo

备注/Memo:

收稿日期:2018-12-02; 修回日期:2019-02-28 投稿网址:http://jese.chd.edu.cn/
基金项目:国家科技重大专项项目(2016ZX05046-005-001); 四川省教育厅重点项目(16ZA0103)
作者简介:王子腾(1994-),男,河北衡水人,理学硕士研究生,E-mail:1849601420@qq.com。
*通讯作者:王 峰(1977-),男,陕西汉中人,副教授,理学博士,博士后,E-mail:wangfeng07@cdut.cn。

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更新日期/Last Update: 2019-05-20