Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化)
依据二维地震剖面的精细地质解释,将塔北沙雅隆起东段自加里东中-晚期以来的断裂活动细分为3期,并对其复合发育过程进行了探讨.研究表明:加里东中-晚期,区内主要发育近NW向的小型逆断层;海西早期,近EW向的压扭断裂开始大规模发育,部分近NW向的断裂也开始扭动,二者呈复合构造样式;海西晚期,区内断裂继承性活动,EW向断裂发生大规模逆冲活动,地层被大幅抬升,并遭受剥蚀.该项研究对于深化塔里木板块北部古生代构造变形研究以及油气勘探等都具有重要的意义....
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Format: | Article |
Language: | zho |
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Zhejiang University Press
2013-09-01
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Series: | Zhejiang Daxue xuebao. Lixue ban |
Subjects: | |
Online Access: | https://doi.org/10.3785/j.issn.1008-9497.2013.05.020 |
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author | WANGWen-xia(王文侠) YAOZe-wei(姚泽伟) ZHENGXiao-li(郑晓丽) HEGuang-yu(何光玉) ZHANGHong-an(张洪安) QILi-xin(漆立新) YUNLu(云露) ZHANGGen-fa(张根法) LINLu(林璐) GUYi(顾忆) |
author_facet | WANGWen-xia(王文侠) YAOZe-wei(姚泽伟) ZHENGXiao-li(郑晓丽) HEGuang-yu(何光玉) ZHANGHong-an(张洪安) QILi-xin(漆立新) YUNLu(云露) ZHANGGen-fa(张根法) LINLu(林璐) GUYi(顾忆) |
author_sort | WANGWen-xia(王文侠) |
collection | DOAJ |
description | 依据二维地震剖面的精细地质解释,将塔北沙雅隆起东段自加里东中-晚期以来的断裂活动细分为3期,并对其复合发育过程进行了探讨.研究表明:加里东中-晚期,区内主要发育近NW向的小型逆断层;海西早期,近EW向的压扭断裂开始大规模发育,部分近NW向的断裂也开始扭动,二者呈复合构造样式;海西晚期,区内断裂继承性活动,EW向断裂发生大规模逆冲活动,地层被大幅抬升,并遭受剥蚀.该项研究对于深化塔里木板块北部古生代构造变形研究以及油气勘探等都具有重要的意义. |
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spelling | doaj.art-25f6fba058f240bbb6201b8f81dfffe72024-03-29T01:58:32ZzhoZhejiang University PressZhejiang Daxue xuebao. Lixue ban1008-94972013-09-0140557457910.3785/j.issn.1008-9497.2013.05.020Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化)WANGWen-xia(王文侠)0YAOZe-wei(姚泽伟)1ZHENGXiao-li(郑晓丽)2HEGuang-yu(何光玉)3ZHANGHong-an(张洪安)4QILi-xin(漆立新)5YUNLu(云露)6ZHANGGen-fa(张根法)7LINLu(林璐)8GUYi(顾忆)9 1. Department of Earth Science, Zhejiang University, Hangzhou 310027, China( 1.浙江大学 地球科学系,浙江 杭州 310027) 1. Department of Earth Science, Zhejiang University, Hangzhou 310027, China( 1.浙江大学 地球科学系,浙江 杭州 310027) 1. Department of Earth Science, Zhejiang University, Hangzhou 310027, China( 1.浙江大学 地球科学系,浙江 杭州 310027) 1. Department of Earth Science, Zhejiang University, Hangzhou 310027, China( 1.浙江大学 地球科学系,浙江 杭州 310027) 2. Northwest Oilfield Company of SINOPEC, Urumqi 830011, China( 2.中国石化西北油田分公司,新疆 乌鲁木齐 830011) 2. Northwest Oilfield Company of SINOPEC, Urumqi 830011, China( 2.中国石化西北油田分公司,新疆 乌鲁木齐 830011) 2. Northwest Oilfield Company of SINOPEC, Urumqi 830011, China( 2.中国石化西北油田分公司,新疆 乌鲁木齐 830011) 2. Northwest Oilfield Company of SINOPEC, Urumqi 830011, China( 2.中国石化西北油田分公司,新疆 乌鲁木齐 830011) 1. Department of Earth Science, Zhejiang University, Hangzhou 310027, China( 1.浙江大学 地球科学系,浙江 杭州 310027) 3. Wuxi Research Institute of Petroleum Geology of SINOPEC, Wuxi 214151, Jiangsu Province, China( 3.中国石化石油勘探开发研究院无锡石油地质研究所,江苏 无锡 214151)依据二维地震剖面的精细地质解释,将塔北沙雅隆起东段自加里东中-晚期以来的断裂活动细分为3期,并对其复合发育过程进行了探讨.研究表明:加里东中-晚期,区内主要发育近NW向的小型逆断层;海西早期,近EW向的压扭断裂开始大规模发育,部分近NW向的断裂也开始扭动,二者呈复合构造样式;海西晚期,区内断裂继承性活动,EW向断裂发生大规模逆冲活动,地层被大幅抬升,并遭受剥蚀.该项研究对于深化塔里木板块北部古生代构造变形研究以及油气勘探等都具有重要的意义.https://doi.org/10.3785/j.issn.1008-9497.2013.05.020复合构造断裂演化古生代沙雅隆起塔里木盆地 |
spellingShingle | WANGWen-xia(王文侠) YAOZe-wei(姚泽伟) ZHENGXiao-li(郑晓丽) HEGuang-yu(何光玉) ZHANGHong-an(张洪安) QILi-xin(漆立新) YUNLu(云露) ZHANGGen-fa(张根法) LINLu(林璐) GUYi(顾忆) Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) Zhejiang Daxue xuebao. Lixue ban 复合构造 断裂演化 古生代 沙雅隆起 塔里木盆地 |
title | Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) |
title_full | Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) |
title_fullStr | Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) |
title_full_unstemmed | Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) |
title_short | Structural features and evolution of Paleozoic faults in Eastern Shaya Uplift, Northern Tarim Basin, NW China(塔北沙雅隆起东段古生代断裂特征及演化) |
title_sort | structural features and evolution of paleozoic faults in eastern shaya uplift northern tarim basin nw china 塔北沙雅隆起东段古生代断裂特征及演化 |
topic | 复合构造 断裂演化 古生代 沙雅隆起 塔里木盆地 |
url | https://doi.org/10.3785/j.issn.1008-9497.2013.05.020 |
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