青西凹陷下白垩统湖相喷流岩成因探讨及其意义

范铭涛; 杨麟科; 方国玉; 汪满福; 李铁锋; 朱利东

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

青西凹陷下白垩统湖相喷流岩成因探讨及其意义

范铭涛, 杨麟科, 方国玉, 汪满福, 李铁锋, 朱利东

文章导航 > 沉积学报 > 2003 > 21(4): 560-564

范铭涛, 杨麟科, 方国玉, 汪满福, 李铁锋, 朱利东. 青西凹陷下白垩统湖相喷流岩成因探讨及其意义[J]. 沉积学报, 2003, 21(4): 560-564.

引用本文:

范铭涛, 杨麟科, 方国玉, 汪满福, 李铁锋, 朱利东. 青西凹陷下白垩统湖相喷流岩成因探讨及其意义[J]. 沉积学报, 2003, 21(4): 560-564.

FAN Ming tao, YANG Ling ke, FANG Guo yu, WANG Man fu, LI Tie feng, ZHU Li dong. Origin of Lacustrine Hydrothermal Sedimentary Rock (Lower Cretaceous) in Qingxi Sag and Its Significance[J]. Acta Sedimentologica Sinica, 2003, 21(4): 560-564.

Citation:

范铭涛, 杨麟科, 方国玉, 汪满福, 李铁锋, 朱利东. 青西凹陷下白垩统湖相喷流岩成因探讨及其意义[J]. 沉积学报, 2003, 21(4): 560-564.

引用本文:

范铭涛, 杨麟科, 方国玉, 汪满福, 李铁锋, 朱利东. 青西凹陷下白垩统湖相喷流岩成因探讨及其意义[J]. 沉积学报, 2003, 21(4): 560-564.

Citation:

青西凹陷下白垩统湖相喷流岩成因探讨及其意义

1.
玉门油田分公司研究院甘肃玉门 735200;
2.
成都理工大学地球科学学院成都 610059

详细信息

作者简介:
范铭涛男 1964 年出生博士地球物理勘探

中图分类号: P588.2

计量

文章访问数: 468
HTML全文浏览量: 7
PDF下载量: 439
被引次数: 0

Origin of Lacustrine Hydrothermal Sedimentary Rock (Lower Cretaceous) in Qingxi Sag and Its Significance

1.
Research Center of Yumen Oilfield Co.Ltd.CNPC, Yumen Gansu 735200;
2.
College of Geosciences, Chengdu Science and Technology University, Chengdu 610059

摘要

摘要: 青西凹陷下白垩统泥云岩 (泥质白云岩、白云质泥岩、白云岩,统称“泥云岩”)以其富含泥级钠长石、石英、铁白云石和重晶石等特殊矿物成分为特点。从构造、沉积、岩石学等方面对青西凹陷下白垩统泥云岩进行了地质分析,指出泥云岩的成因与湖底热水喷流有关。
- 青西凹陷 /
- 泥级钠长石 /
- 泥云岩 /
- 热水矿物 /
- 喷流岩
Abstract: Lower Cretaceous muddy dolostone distributed Qingxi sag, Jiuxi depression is characterized by the high content of special mineral assemblage including clay-sized albite and quartz, ankerite and barite, and so on.So far, there have been different debates on the origin of this special rock type, resulting in the difficult evaluation on the muddy dolostone reservoir.Based on the systematic structural, depositional and petrologic study on this kind of rock, this paper has pointed out that the rock is closely related to the overflow of thermal water from lake bottom, and, furthermore, discusses the role of the special rock in controlling petroleum formation as well as the future exploration direction.
- Qing xi sag /
- clay-sized albite /
- muddy dolostone /
- thermal water minerals /
- thermal fluid rock

HTML全文

参考文献(13)

[1]	杨经绥,孟繁聪,张建新.重新认识阿尔金断裂东段红柳峡火山岩的时代及构造意义[J].中国科学(D辑), 2001,31(增刊): 12 [Yang J S, Meng F C, Zhang J X. Recognition of the geologic age of volcanic rock distributed in the eastern end of Hongliuxia Fault and its tectonic significance [J]. Science in China (series D), 2001, 31(Suppl.):12]
[2]	肖容阁,李朝阳.热水成矿作用[J]. 地学前缘,1994, 1(3～4):10[Xiao R G, Li C Y. Thermal ore genesis [J]. Geoscience Frontier, 1994,1(3～4):10]
[3]	解习农,李思田等. 热流体活动示踪标志及其地质意义[J]. 地球科学-中国地质大学学报,1999,24(2):3 [Xie X N, Li S T, et al. Tracing indicators for thermal fluid activity and its geological significance[J]. Geosciences-Journal of China University of Geosciences, 1999, 24(2):3]
[4]	周永章,刘建明,陈多福.华南古海洋热水沉积作用研究概述及若干认识[J]. 矿物岩石地球化学通报,2000,19(2):4 [Zhou Y Z, Liu J M, Chen D F. Review of paleomarine thermal sedimentation in the south China [J]. Bulletin of Mineral, Rock and Geochemistry, 2000,19(2):4]
[5]	吴志亮,李峰. 热水沉积成岩成矿作用-以阿尔泰泥盆纪火山沉积盆地为例[M]. 北京:地质出版社,1996[Wu Z L, Li F. Thermal sedimentation, diagenesis and ore deposit processs-taking Devonian volcanic basin in Aretai as an example [M]. Beijing: Geological Publishing House,1996]
[6]	Bischoff J L. Red sea geothermal brine deposits[A]. In: Degens E T and Ross D A, eds. Hot brines and recent heavy metal deposits of the Red sea[C]. New York: Springer-Verlag, 1969.338～401
[7]	Stoffers P and Botz R. Formation of hydrothermal carbonate in Lake Tanganyika, East-Central Africa[J]. Chemical Geology, 1994, 115( 1～2): 117～122
[8]	Simoneit B R T, Lonsdale P F. Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin[J]. Nature, 1982, 295:198～202
[9]	Didyk B M, Simoneit B R T. Hydrothermal oil of Guaymas Basin and implications for petroleum formation mechanisms[J]. Nature, 1989,342:65～69
[10]	Yamanaka T, Ishibashi J, Hashimoto J. Organic geochemistry of hydrothermal petroleum generated in the submarine Wakamiko Caldera, southern Kyushu Japan[J]. Organic Geochemistry, 2000, 31:1 117～1 132
[11]	Simoneit B R T, Fetzer J C. High molecular weight polycyclic aromatic hydrocarbons in hydrothermal petroleums from the gulf of Califonia and northeast Pacific Ocean[J]. Organic Geochemistry, 1996,24: 1 065～1 077
[12]	Simoneit B R T. Hydrothermal petroleum: genesis, migration, and deposition in Guaymas basin. Gulf of California[J]. Canadian Journal of Earth Science, 1985, 22: 1 919～1 929
[13]	Tiercelin J J, Thouin C, Kalala T. Discovery of sublacustrine hydrothermal activity and associated massive sulfides and hydrocarbons in the north Tanganyika trough, east African Rift[J]. Geology, 17: 1 053～1 056