DOI: 10.1007/s00531-012-0794-z
Scopus记录号: 2-s2.0-84872332555
论文题名: Fault damage zone origin of the Teufelsmauer, Subhercynian Cretaceous Basin, Germany
作者: Klimczak C. ; Schultz R.A.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2013
卷: 102, 期: 1 起始页码: 121
结束页码: 138
语种: 英语
英文关键词: Deformation bands
; Fault damage zone
; Harz Mountains
; Teufelsmauer
Scopus关键词: basin evolution
; cementation
; damage
; deformation
; fault zone
; kinematics
; sandstone
; strain
; tectonic evolution
; Germany
; Harz Mountains
英文摘要: 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. URL: 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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资源类型: 期刊论文
标识符: 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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作者单位: 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)