Zobrazeno 1 - 10
of 90
pro vyhledávání: '"Ute Weckmann"'
Autor:
Laura V. Krone, Ferdinand J. Hampl, Christopher Schwerdhelm, Casey Bryce, Lars Ganzert, Axel Kitte, Kirstin Übernickel, Armin Dielforder, Santiago Aldaz, Rómulo Oses-Pedraza, Jeffrey Paulo H. Perez, Pablo Sanchez-Alfaro, Dirk Wagner, Ute Weckmann, Friedhelm von Blanckenburg
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Abstract The weathering front is the boundary beneath Earth’s surface where pristine rock is converted into weathered rock. It is the base of the “critical zone”, in which the lithosphere, biosphere, and atmosphere interact. Typically, this fro
Externí odkaz:
https://doaj.org/article/127a87e9c54f4c688f95e83536c76b35
Autor:
Maarten de Wit, Harald Furnes, Scott MacLennan, Moctar Doucouré, Blair Schoene, Ute Weckmann, Uma Martinez, Sam Bowring
Publikováno v:
Geoscience Frontiers, Vol 9, Iss 3, Pp 603-665 (2018)
The Makhonjwa Mountains, traditionally referred to as the Barberton Greenstone Belt, retain an iconic Paleoarchean archive against which numerical models of early earth geodynamics can be tested. We present new geologic and structural maps, geochemic
Externí odkaz:
https://doaj.org/article/31ea213e5f5f421b8225ca4386ea3c3e
The Radio-Magnetotelluric (RMT) method is a geophysical near-surface imaging technique with a broad range of possible applications. In 2020, the GFZ Potsdam has acquired a newly developed horizontal magnetic dipole transmitter that allows the applica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a870d48b7bb70e043c21ce5cd40d9cb
https://doi.org/10.5194/egusphere-egu23-917
https://doi.org/10.5194/egusphere-egu23-917
The Bohemian Massif is part of the geodynamically active European Cenozoic Rift System and represents its easternmost termination. The study area is situated at the junction of three different Variscan tectonic units and hosts beside the Eger Rift a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a99111c555e9e59c81f9de2a48c05682
https://doi.org/10.5194/egusphere-egu22-4884
https://doi.org/10.5194/egusphere-egu22-4884
Autor:
José Cruces-Zabala, Oliver Ritter, Ute Weckmann, Kristina Tietze, Naser Meqbel, Franck Audemard, Michael Schmitz
Publikováno v:
Journal of South American Earth Sciences
The 100 km wide Mérida Andes extend from the Colombian/Venezuelan border to the Coastal Cordillera. The mountain chain and its associated major strike-slip fault systems in western Venezuela formed due to oblique convergence of the Caribbean with th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c8fc44fe7666686491c6fc0903accef
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011454
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011454
Publikováno v:
Malehmir, A, Manzi, M, Draganov, D, Weckmann, U & Auken, E 2020, ' Introduction to the special issue on “Cost-effective and innovative mineral exploration solutions” ', Geophysical Prospecting, vol. 68, no. 1, pp. 3-6 . https://doi.org/10.1111/1365-2478.12915
Geophysical Prospecting
Geophysical Prospecting
The mineral exploration industry is again in a boom to provide new resources of critical raw materials as well as base and precious metals. This is evident from the globally increased expenditure reported for 2018 (International Mining 2018). Global
Autor:
Anna Platz, Ute Weckmann, Josef Pek, Světlana Kováčiková, Radek Klanica, Johannes Mair, Basel Aleid
Publikováno v:
Tectonophysics
The region of West Bohemia and Upper Palatinate belongs to the West Bohemian Massif. The study area is situated at the junction of three different Variscan tectonic units and hosts the ENE-WSW trending Ohře Rift as well as many different fault syste
The Mérida Andes are a 100 km wide mountain chain that extends from the Colombian/Venezuelan border to the Caribbean coast. To the north and south, the Mérida Andes are bound by hydrocarbon-rich sedimentary basins. Uplift of the mountains started i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::608f9eddc26ac46d66b10a62ef2512aa
https://doi.org/10.5194/egusphere-egu21-15040
https://doi.org/10.5194/egusphere-egu21-15040
Autor:
Johannes Mair, Ute Weckmann, Radek Klanica, Basel Aleid, Anna Platz, Paula Rulff, Svetlana Kováčiková, Gregor Willkommen
The Bohemian Massif represents the easternmost part of the geodynamically active European Cenozoic Rift System. This region hosts the contact between three tectonic units of the Variscan Belt, the NE-SW trending Eger Rift and the NNW-SSE striking Mar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e9fff355e82158d1d68c30554bbeea8
https://doi.org/10.5194/egusphere-egu21-12081
https://doi.org/10.5194/egusphere-egu21-12081
Autor:
Ute Weckmann, Lars Ganzert, Jeffrey Paulo H. Perez, Santiago Aldaz, Ferdinand Hampl, Christopher Schwerdhelm, Pablo Sanchez-Alfaro, Laura V. Krone, Rómulo Oses-Pedraza, Dirk Wagner, Armin Dielforder, Axel Kitte, Friedhelm von Blanckenburg, Casey Bryce, Kirstin Übernickel
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
The weathering front, the boundary beneath Earth’s surface where unweathered bedrock is converted into weathered rock, is the base of the critical zone. Typically, this front is located no more than 20 m deep in granitoid rock in humid climate zone
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32eac97429e1aa045c7e9176d6998fb5
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006658_1/component/file_5007108/5006658.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006658_1/component/file_5007108/5006658.pdf