Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryMineral Visual ExplorerAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral QuizTime Machine
Photo SearchPhoto GalleriesSearch by ColorPhoto Colour ExplorerNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Dang, Jiaxiang, Zhou, Yongsheng (2021) Amorphous materials and clay mineral formation in the coseismic gouge from a surface rupture of the Ms 8.0 Wenchuan earthquake. Tectonophysics, 818. 229077 doi:10.1016/j.tecto.2021.229077

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleAmorphous materials and clay mineral formation in the coseismic gouge from a surface rupture of the Ms 8.0 Wenchuan earthquake
JournalTectonophysics
AuthorsDang, JiaxiangAuthor
Zhou, YongshengAuthor
Year2021 (November)Volume818
PublisherElsevier BV
DOIdoi:10.1016/j.tecto.2021.229077Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID15463582Long-form Identifiermindat:1:5:15463582:4
GUID0
Full ReferenceDang, Jiaxiang, Zhou, Yongsheng (2021) Amorphous materials and clay mineral formation in the coseismic gouge from a surface rupture of the Ms 8.0 Wenchuan earthquake. Tectonophysics, 818. 229077 doi:10.1016/j.tecto.2021.229077
Plain TextDang, Jiaxiang, Zhou, Yongsheng (2021) Amorphous materials and clay mineral formation in the coseismic gouge from a surface rupture of the Ms 8.0 Wenchuan earthquake. Tectonophysics, 818. 229077 doi:10.1016/j.tecto.2021.229077
In(2021) Tectonophysics Vol. 818. Elsevier BV

See Also

These are possibly similar items as determined by title/reference text matching only.

Dang, Jiaxiang, Zhou, Yongsheng (2023) Structural fabrics of carbon grains in a natural fault gouge reactivated by the 2008 Wenchuan earthquake. Terra Nova, 35 (2) 91-100 doi:10.1111/ter.12633
Macklin, Clarrie, Kaneko, Yoshihiro, Kearse, Jesse (2021) Coseismic slickenlines record the emergence of multiple rupture fronts during a surface-breaking earthquake. Tectonophysics, 808. 228834 doi:10.1016/j.tecto.2021.228834
Liu, Yaowei, Chen, Tao, Xie, Furen, Du, Fang, Yang, Duoxing, Zhang, Lei, Xu, Liqing (2014) Analysis of fluid induced aftershocks following the 2008 Wenchuan Ms 8.0 earthquake. Tectonophysics, 619. 149-158 doi:10.1016/j.tecto.2013.09.010
Xu, Zheng; Li, Yong; Yi, Guixi; Peng, Liyuan; Yang, Xin; Wen, Wanzhang; Zhao, Shaoze (2026) Numerical simulation of stress transfer and triggered earthquake prediction along the Longmenshan-Foreland Basin driven by the Wenchuan Ms 8.0 earthquake. Tectonophysics, 918. doi:10.1016/j.tecto.2025.230972
Dang, Jiaxiang, Zhou, Yongsheng, He, Changrong, Ma, Shengli (2018) Mineralogical compositions of fault rocks from surface ruptures of Wenchuan earthquake and implication of mineral transformation during the seismic cycle along Yingxiu-Beichuan fault, Sichuan Province, China. Mineralogy and Petrology, 112 (3) 341-355 doi:10.1007/s00710-017-0546-7
Hashimoto, Manabu, Enomoto, Mari, Fukushima, Yo (2010) Coseismic Deformation from the 2008 Wenchuan, China, Earthquake Derived from ALOS/PALSAR Images. Tectonophysics, 491 (1) 59-71 doi:10.1016/j.tecto.2009.08.034
Medina Luna, Lorena, Hetland, Eric A. (2013) Regional stresses inferred from coseismic slip models of the 2008 Mw 7.9 Wenchuan, China, earthquake. Tectonophysics, 584. 43-53 doi:10.1016/j.tecto.2012.03.027
Li, Yong, Huang, Runqiu, Yan, Liang, Densmore, Alexander L., Zhou, Rongjun (2010) Surface Rupture and Hazard of Wenchuan Ms 8.0 Earthquake, Sichuan, China. International Journal of Geosciences, 1 (1). 21-31 doi:10.4236/ijg.2010.11003
Li, Chuan-You, Wei, Zhan-Yu, Ye, Jian-Qing, Han, Yong-Bing, Zheng, Wen-Jun (2010) Amounts and styles of coseismic deformation along the northern segment of surface rupture, of the 2008 Wenchuan Mw 7.9 earthquake, China. Tectonophysics, 491 (1) 35-58 doi:10.1016/j.tecto.2009.09.023
Zhu, Shoubiao, Zhang, Peizhen (2013) FEM simulation of interseismic and coseismic deformation associated with the 2008 Wenchuan Earthquake. Tectonophysics, 584. 64-80 doi:10.1016/j.tecto.2012.06.024
Sayab, Mohammad, Khan, Muhammad Asif (2010) Temporal evolution of surface rupture deduced from coseismic multi-mode secondary fractures: Insights from the October 8, 2005 (Mw 7.6) Kashmir earthquake, NW Himalaya. Tectonophysics, 493 (1) 58-73 doi:10.1016/j.tecto.2010.07.001
 
and/or  
Mindat.org® is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. Mindat® and mindat.org® are registered trademarks of the Hudson Institute of Mineralogy.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2026, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph and Ida Chau.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: June 4, 2026 21:45:00
Go to top of page