F
Friedemann Wenzel
Researcher at Karlsruhe Institute of Technology
Publications - 225
Citations - 7090
Friedemann Wenzel is an academic researcher from Karlsruhe Institute of Technology. The author has contributed to research in topics: Crust & Population. The author has an hindex of 41, co-authored 224 publications receiving 6312 citations. Previous affiliations of Friedemann Wenzel include University of Oslo & Macquarie University.
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Partially Molten Middle Crust Beneath Southern Tibet: Synthesis of Project INDEPTH Results
K. D. Nelson,Wenjin Zhao,Lawrence D. Brown,J. Kuo,Jinkai Che,Xianwen Liu,Simon L. Klemperer,Yizhaq Makovsky,Rolf Meissner,James Mechie,Rainer Kind,Friedemann Wenzel,James Ni,J. Nabelek,Chen Le-shou,Handong Tan,Wenbo Wei,Alan G. Jones,John R. Booker,Martyn Unsworth,William S.F. Kidd,M. Hauck,Douglas Alsdorf,A. Ross,M. Cogan,Changde Wu,Eric Sandvol,M. A. Edwards +27 more
TL;DR: The results suggest that during Neogene time the underthrusting Indian crust has acted as a plunger, displacing the molten middle crust to the north while at the same time contributing to this layer by melting and ductile flow.
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The World Stress Map database release 2016 : Crustal stress pattern across scales
Oliver Heidbach,Mojtaba Rajabi,Xiaofeng Cui,Karl Fuchs,Birgit Müller,John Reinecker,Karsten Reiter,Mark Tingay,Friedemann Wenzel,Furen Xie,Moritz Ziegler,Mary-Lou Zoback,Mark D. Zoback +12 more
TL;DR: In this article, the authors present details of the new WSM database release 2016 and an analysis of global and regional stress pattern, and show two examples of 40 degrees-60 degrees S-Hmax rotations within 70 km.
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Direct mapping of seismic data to the domain of intercept time and ray parameter—A plane‐wave decomposition
TL;DR: In this paper, a plane-wave decomposition based on beam forming of wide-aperture seismic array data is used to determine automatically the loci of coherent seismic reflection and refraction events.
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Seismogenic index and magnitude probability of earthquakes induced during reservoir fluid stimulations
TL;DR: In this article, the authors proposed a nonlinear relaxation process in the pore fluid of the Earth's crust, where the tectonic stress in the crust is close to critical stress, causing brittle failure of rocks.
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Plate boundary forces are not enough: Second‐ and third‐order stress patterns highlighted in the World Stress Map database
Oliver Heidbach,John Reinecker,Mark Tingay,Birgit Müller,Blanka Sperner,Karl Fuchs,Friedemann Wenzel +6 more
TL;DR: The World Stress Map Project (WSMP) database as mentioned in this paper provides a global database of contemporary tectonic stress information of the Earth's crust, and the 2005 release of the WSMP database provides, for some areas, high data density that enables us to investigate third-order (local) stress field variations and forces controlling them such as active faults, local inclusions, detachment horizons, and density contrasts.