globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-012-0794-z
Scopus ID: 2-s2.0-84872332555
Title:
Fault damage zone origin of the Teufelsmauer, Subhercynian Cretaceous Basin, Germany
Author: Klimczak C.; Schultz R.A.
Source Publication: International Journal of Earth Sciences
ISSN: 14373254
Publishing Year: 2013
Volume: 102, Issue:1
pages begin: 121
pages end: 138
Language: 英语
Keyword: Deformation bands ; Fault damage zone ; Harz Mountains ; Teufelsmauer
Scopus Keyword: basin evolution ; cementation ; damage ; deformation ; fault zone ; kinematics ; sandstone ; strain ; tectonic evolution ; Germany ; Harz Mountains
English Abstract: Recognition of fractures as porosity-reducing deformation bands pervading all sandstone segments of the Teufelsmauer, Subhercynian Creatceous Basin, Germany, motivates a study relating the observed macroscopic and microscopic deformation to the damage zone of the nearby Harz border fault. Deformation bands, confirmed and documented by several porosity-reducing micro-mechanisms, such as cataclasis, particulate flow, pressure solution and a heavy quartz cementation, were mapped and analyzed in terms of the kinematics and deformation intensities expressed by them. Deformation band kinematics are uniform throughout the entire basin and consistent with the large-scale tectonic structures of the area. A strain intensity study highlights two narrow but long zones of deformation bands, sub-parallel to the Harz border fault. Deformation band kinematics, strain intensity, as well as micro-mechanisms are all consistent with a continuous but internally diverse deformation band damage zone of the entire Teufelsmauer structure along the Harz border fault, bringing new insights into the tectonic evolution and the origin of the heavy quartz cementation of the sandstones in the Subhercynian Cretaceous Basin. © 2012 Springer-Verlag.
Related Link: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84872332555&doi=10.1007%2fs00531-012-0794-z&partnerID=40&md5=f1dafb1823534a7533ea1d8d89eba347
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被引频次[WOS]:6   [查看WOS记录]     [查看WOS中相关记录]
Document Type: 期刊论文
Identifier: http://119.78.100.158/handle/2HF3EXSE/70587
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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Affiliation: Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, N.W., WA, DC 20015-1305, United States; ConocoPhillips, Geological Technology, PR2010, 600 North Dairy Ashford, Houston, TX, 77079, United States

Recommended Citation:
Klimczak C.,Schultz R.A.. Fault damage zone origin of the Teufelsmauer, Subhercynian Cretaceous Basin, Germany[J]. International Journal of Earth Sciences,2013-01-01,102(1)
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