云南宁蒗新生代盆地的形成与演化

doi:10.19388/j.zgdzdc.2021.01.09

Abstract
Figure/Table
References
Related Citation (15)

Download: PDF (8295 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Ninglang Basin is located on the active edge of Yangtze Paleo-Continent Block,and it is a structural transformation zone, which absorbed and regulated the stress and strain of India-Eurasia collision. In order to study the relationship between the formation and evolution of Cenozoic basins in Ninglang area of Yunnan Province and its regional structures and basin types, the authors analyzed the structural framework of Ninglang Basin and its adjacent areas, through several 1:50 000 regional geological surveys. The results show that the formation and evolution of the basin are controlled by faults. Ninglang Basin is believed to be a typical strike-slip pull-apart basin through the study of the sedimentary construction, spatial evolution of the basin-controlling structure and the regional geological background. The evolution has gone through three stages: pulling apart and opening stage from the Paleocene to Eocene, pull-apart basin deposition stage from the beginning of the Eocene to the end of the Eocene, and the basin reform stage from the Eocene to the Miocene.

Key words： Ninglang Cenozoic basin Paleogene strike-slip pull-apart basin evolution

Received: 11 May 2020

:	P546
	P542.3

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	MA Changwei
	YE Zhengyu
	CAO Yun
	WANG Chao

Cite this article:

MA Changwei,YE Zhengyu,CAO Yun, et al. Formation and evolution of Cenozoic basin in Ninglang of Yunnan Province[J]. , 2021, 8(1): 80-88.

URL:

http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2021.01.09 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2021/V8/I1/80

[1] 潘桂堂,肖庆辉,陆松年,等.中国大地构造单元划分[J].中国地质,2009,36(1):1-28.
Pan G T,Xiao Q H,Lu S N,et al.Subdivision of tectonic units in China[J].Geology in China,2009,36(1):1-28.
[2] 张远泽. 川滇地块东部主要活动断裂新生代精确构造年代格架及其对青藏高原东缘新生代动力学过程的启示[D].武汉:中国地质大学(武汉),2015.
Zhang Y Z.Tectonic chronology constraint on the faults bounding the east Sichuan-Yunnan block and implications for Tibetan Plateau kinetics[D].Wuhan:China University of Geosciences(Wuhan),2015.
[3] 侯增谦,潘桂堂,王安建,等.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质,2006,25(5):521-543.
Hou Z Q,Pan G T,Wang A J,et al.Metallogenesis in Tibetan collisional orogenic belt:Ⅱ.Mineralization in late collisional transformation setting[J].Mineral Deposits,2006,25(5):521-543.
[4] 钟大赉. 滇川西部古特提斯造山带[M].北京:北京科学出版社,1998:1-231.
Zhong D L.The Ancient Tethys Orogenic Belt in Western Yunnan and Sichuan[M].Beijing:Beijing Science and Technology Press,1998:1-231.
[5] 谭筱虹. 滇西三江地区新生代构造盆地的特征及形成机制[J].云南地质,1999,18(2):112-121.
Tan X H.Features and formation mechanism of Cenozoic tectonic basins in the Sanjiang area of western Yunnan[J].Yunnan Geology,1999,18(2):112-121.
[6] 王振华. 宁蒗盆地油气勘探远景分析[J].云南地质,2000,19(4):443-448.
Wang Z H.An analysis of oil-gas exploration prospective of Ninglang Basin[J].Yunnan Geology,2000,19(4):443-448.
[7] 董林. 宁蒗盆地油气勘探有利区分析[J].能源与环保,2017,39(2):155-159.
Dong L.Analysis on advantageous area of oil and gas exploration in Ninglang Basin[J].China Energy and Environmental Protection,2017,39(2):155-159.
[8] 叶征宇,马昌威.1:50 000灵源幅、大厂幅、腊姑河幅区域地质调查报告[R].北京:中国地质调查局,2019.
Ye Z Y,Ma C W.Regional Geological Survey Report of the Lingyuan Sheet,Dachang Sheet and Laguhe Sheet of 1:50 000[R].Beijing:China Geological Survey,2019.
[9] 张锦让,王宏.1:50 000宁蒗幅、西布河乡幅、波罗幅区域地质调查报告[R].北京:中国地质调查局,2019.
Zhang J R,Wang H.Regional Geological Survey Reports of the Ninglang Sheet,Xibuhe Township Sheet and Boluo Sheet of 1:50 000[R].Beijing:China Geological Survey,2019.
[10] 王宝碌,吕世琨,胡居贵.试论川滇黔菱形地块[J].云南地质,2004,23(2):140-153.
Wang B L,Lu S K,Hu J G.A tentative description of the Chuan-Dian-Qian rhombic massif[J].Yunnan Geology,2004,23(2):140-153.
[11] 郭永生. 试论金河—菁河断裂走滑特征[J].四川地质学报,1986(2):39-42.
Guo Y S.On the strike-slip characteristics of the Jinhe-Qinghe fault[J].Acta Geological Sichuan,1986(2):39-42.
[12] 潘桂棠,徐强,侯增谦,等.西南"三江"多岛弧造山过程成矿系统与资源评价[M].北京:地质出版社,2003.
Pan G T,Xu Q,Hou Z Q,et al.Mineralization System and Resource Evaluation of the Nujiang-Lancangjiang-Jinshajiang Multi-Island Arc Orogenic Process in Southwestern China[M].Beijing:Geological Publishing Honse,2003.
[13] 肖龙,徐义刚,梅厚钧,等.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系——地球化学证据[J].岩石学报,2003,19(1):38-48.
Xiao L,Xu Y G,Mei H J,et al.Late Permian flood basalts at Jinping area and its relation to Emei mantle plume:geochemical evidences[J].Acta Petrologica Sinica,2003,19(1):38-48.
[14] 朱民. 上扬子西南地区三叠系沉积记录及其对盆山格局的制约[D].杭州:浙江大学,2016.
Zhu M.The depositional record of Southwestern Upper Yangtze area during Triassic and its restriction on the tectonic framework of basin and range[D].Hangzhou:Zhejiang University,2016.
[15] 尹福光,潘桂棠,万方,等.西南"三江"造山带大地构造相[J].沉积与特提斯地质,2006,26(4):33-39.
Yin F G,Pan G T,Wan F,et al.Tectonic facies along the Nujiang-Lancangjiang-Jinshajiang orogenic belt in southwestern China[J].Sedimentary Geology and Tethyan Geology,2006,26(4):33-39.
[16] 邓军,侯增谦,莫宣学,等.三江特提斯复合造山与成矿作用[J].矿床地质,2010,29(1):37-42.
Deng J,Hou Z Q,Mo X X,et al.Superimposed orogenesis and metallogenesis in Sanjiang Tethys[J].Mineral Deposits,2010,29(1):37-42.
[17] 李文昌,潘桂棠,侯增谦,等.西南"三江"多岛弧盆-碰撞造山成矿理论与勘查技术[M].北京:地质出版社,2010.
Li W C,Pan G T,Hou Z Q,et al.Southwest "Sanjiang" Multi-Island Arc Basin-Collision Orogeny and Mineralization Theory and Exploration Technology[M].Beijing:Geological Publishing House,2010.
[18] 许志琴,王勤,李忠海,等.印度-亚洲碰撞:从挤压到走滑的构造转换[J].地质学报,2016,90(1):1-23.
Xu Z Q,Wang Q,Li Z H,et al.Indo-Asian collision:Tectonic transition from compression to strike-slip[J].Acta Geology Sinica,2016,90(1):1-23.
[19] 李静,张志斌,熊家镛,等.云南省成矿地质背景研究报告[M].昆明:云南科技出版社,2003.
Li J,Zhang Z B,Xiong J Y,et al.Yunnan Province Metallogenic Geological Background Research Report[M].Kunming:Yunnan Science and Technology Press,2003.
[20] 胡受权,曹运江,郭文平.云南宁蒗地区喜山期斑岩成矿带地质特征[J].昆明理工大学学报,1998,23(6):116-123.
Hu S Q,Cao Y J,Guo W P.Geological characteristics of the metallogenic series of Hymalayan porphyry belt in Ninglang district,Yunnan[J].Journal of Kunming University of Science and Technology,1998,23(6):116-123.
[21] 徐恒,崔银亮,周家喜,等.云南永胜分水岭矿区富碱斑岩地球化学、锆石U-Pb年龄及其地质意义[J].大地构造与成矿学,2016,40(3):614-624.
Xu H,Cui Y L,Zhou J X,et al.The geochemistry of alkali-rich porphyry,zircon U-Pb age and its geological significance in Fenshuiling mining area,Yongsheng,Yunnan[J].Geotectonica et Metallogenia,2016,40(3):614-624.