Strain and kinematic vorticity analysis: An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone, western Yunnan, China | |
Zhang Bo1; Zhang JinJiang2; Zhong DaLai1; Guo Lei2 | |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES |
2009-05-01 | |
卷号 | 52期号:5页码:602-618 |
关键词 | strain kinematic vorticity transpression strain partitioning Lancangjiang shear zone |
ISSN号 | 1006-9313 |
DOI | 10.1007/s11430-009-0065-4 |
文献子类 | Article |
英文摘要 | This work deals with the preliminary relationship between strain path and strain partitioning pattern in a sinistral transpressional zone, Lancangjiang shear zone, located to the southeast of Tibet. Various ductile rocks provide an opportunity to investigate quantitative finite strain (R (s)), kinematic vorticity values (W (m) ), and proportions of simple and pure shear components. The mean kinematic vorticity values (W (m) ) were evaluated based on three methods, such as R (s)-theta, prophyroclast hyperbolic distribution method (PHD), and polar Mohr diagram construction (PMD). W (m) for mylonitic metasediments of the low-grade schist belt ranged from 0.19 to 0.54. Protomylonites, mylonites, and ultramylonites recorded differential W (m) values, 0.19-0.73, 0.11-0.8, and 0.84-0.95 (even 0.99) respectively in the high-grade gneiss belt. Based on classical strain analysis and these kinematic vorticity evaluations, the shear zone is classified as a preliminarily bulk monoclinic symmetry. The pattern of vorticity path suggests that a previously undocumented transpressional setting and strain partitioning pattern in the southeast region of Tibet Plateau, characterized by steep-narrow domain of simple-shearing (Tertiary strike-slip shearing) deformation and wider domain of mostly pure-shearing (Tertiary contraction) to accommodate intracontinental deformation. |
WOS关键词 | METAMORPHIC CORE COMPLEX ; INDO-CHINA ; SAMBAGAWA BELT ; SW JAPAN ; SE ASIA ; DEFORMATION ; TECTONICS ; EXTRUSION ; MYANMAR ; MODEL |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000265924500003 |
资助机构 | National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; 49802020 ; 49802020 ; 49802020 ; 49802020 ; 40172074) ; 40172074) ; 40172074) ; 40172074) ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; 49802020 ; 49802020 ; 49802020 ; 49802020 ; 40172074) ; 40172074) ; 40172074) ; 40172074) ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; 49802020 ; 49802020 ; 49802020 ; 49802020 ; 40172074) ; 40172074) ; 40172074) ; 40172074) ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; National Natural Science Foundation of China(40802050 ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; China Postdoctoral Science Foundation(20070440065) ; 49802020 ; 49802020 ; 49802020 ; 49802020 ; 40172074) ; 40172074) ; 40172074) ; 40172074) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/70266] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zhang Bo |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang Bo,Zhang JinJiang,Zhong DaLai,et al. Strain and kinematic vorticity analysis: An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone, western Yunnan, China[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2009,52(5):602-618. |
APA | Zhang Bo,Zhang JinJiang,Zhong DaLai,&Guo Lei.(2009).Strain and kinematic vorticity analysis: An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone, western Yunnan, China.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,52(5),602-618. |
MLA | Zhang Bo,et al."Strain and kinematic vorticity analysis: An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone, western Yunnan, China".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 52.5(2009):602-618. |
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