Detachment faulting and late Paleozoic epithermal Ag-base-metal mineralization in the Spanish central system
1988; Geological Society of America; Volume: 16; Issue: 9 Linguagem: Inglês
10.1130/0091-7613(1988)016 2.3.co;2
ISSN1943-2682
AutoresMiguel Doblas, Roberto Oyarzun, Rosario Lunar Hernández, Nicolás Mayor, J. Julio Camarero,
Tópico(s)Geomagnetism and Paleomagnetism Studies
ResumoResearch Article| September 01, 1988 Detachment faulting and late Paleozoic epithermal Ag-base-metal mineralization in the Spanish central system Miguel Doblas; Miguel Doblas 1Departamento de Geodinámica Interna, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar Roberto Oyarzun; Roberto Oyarzun 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar Rosario Lunar; Rosario Lunar 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar Nicolas Mayor; Nicolas Mayor 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Search for other works by this author on: GSW Google Scholar Jesus Martinez Jesus Martinez 3Museo Nacional de Ciencias Naturales, Consejo Superior de Investigaciones Científicas, Madrid, Spain Search for other works by this author on: GSW Google Scholar Author and Article Information Miguel Doblas 1Departamento de Geodinámica Interna, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Roberto Oyarzun 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Rosario Lunar 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Nicolas Mayor 2Departamento de Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense, 28040 Madrid, Spain Jesus Martinez 3Museo Nacional de Ciencias Naturales, Consejo Superior de Investigaciones Científicas, Madrid, Spain Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1988) 16 (9): 800–803. https://doi.org/10.1130/0091-7613(1988)016 2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Miguel Doblas, Roberto Oyarzun, Rosario Lunar, Nicolas Mayor, Jesus Martinez; Detachment faulting and late Paleozoic epithermal Ag-base-metal mineralization in the Spanish central system. Geology 1988;; 16 (9): 800–803. doi: https://doi.org/10.1130/0091-7613(1988)016 2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Hydrothermal activity during late Hercynian time resulted in epithermal silver-base-metal (Pb-Zn-Cu) vein formation in the eastern part of the Spanish central system. During the Hercynian orogeny, the central Iberian crust was thickened by compressional tectonics, heated, weakened, and subsequently overthickened by massive late Hercynian granitic intrusions. Subsequently, the central Iberian crustal welt underwent extensional collapse through lithosphere-scale, low-angle detachment faulting. The detachment systems evolved through tectonic denudation, isostatic rebound, and upward arching to define an extensional province much like the U.S. Basin and Range. Andesitic volcanism and hydrothermal activity occurred during extension, inducing epithermal-type hydrothermal convecting systems that leached, transported, and precipitated silver and base metals along fractures crosscutting the Hiendelaencina metamorphic core complex. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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