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High rates of arc consumption by subduction processes: Some consequences
Abstract
Research Article| September 01, 1995 Crustal history of Margarita Island (Venezuela) in detail: Constraint on the Caribbean plate-tectonic scenario Bernhard Stöckhert; Bernhard Stöckhert 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Search for other works by this author on: GSW Google Scholar Walter V. Maresch; Walter V. Maresch 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Search for other works by this author on: GSW Google Scholar Manfred Brix; Manfred Brix 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Search for other works by this author on: GSW Google Scholar Claudia Kaiser; Claudia Kaiser 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Search for other works by this author on: GSW Google Scholar Andreas Toetz; Andreas Toetz 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Search for other works by this author on: GSW Google Scholar Rolf Kluge; Rolf Kluge 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Search for other works by this author on: GSW Google Scholar Gabriela Krückhans-Lueder Gabriela Krückhans-Lueder 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Search for other works by this author on: GSW Google Scholar Author and Article Information Bernhard Stöckhert 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Walter V. Maresch 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Manfred Brix 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Claudia Kaiser 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Andreas Toetz 1Institut für Geologie, Ruhr-Universität Bochum, Postfach 102148, D-44721 Bochum, Germany Rolf Kluge 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Gabriela Krückhans-Lueder 2Institut für Mineralogie, Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1995) 23 (9): 787–790. https://doi.org/10.1130/0091-7613(1995)023<0787:CHOMIV>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 Bernhard Stöckhert, Walter V. Maresch, Manfred Brix, Claudia Kaiser, Andreas Toetz, Rolf Kluge, Gabriela Krückhans-Lueder; Crustal history of Margarita Island (Venezuela) in detail: Constraint on the Caribbean plate-tectonic scenario. Geology 1995;; 23 (9): 787–790. doi: https://doi.org/10.1130/0091-7613(1995)023<0787:CHOMIV>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 The pressure-temperature-time-deformation evolution for the crust of Margarita Island (Venezuela) has been established to allow comparison with current plate-tectonic models for the Caribbean region. On Margarita, the 12 recognizable stages of development can be summarized in terms of the following evolving tectonic settings: Protolith evolution as Aptian-Albian or older oceanic crust, as well as continental crust with Paleozoic basement (stages 1 and 2); accretion and high-pressure metamorphism (500–600 °C, 10–14 kbar) as the Margarita Complex in the deep level of a fore arc at 100–90 Ma (stage 3); ascent, cooling, and emplacement into the intermediate crustal level of a volcanic arc at 90–80 Ma (stage 4); transform plate-margin setting at a comparable level at 80–50 Ma (stage 5); second episode of rapid uplift and cooling (stages 6 and 7); and shallow crustal level close to transform plate margin from 50 Ma to present (stages 8 to 12). This complex sequence is in excellent agreement with plate-tectonic scenarios that require a Pacific origin for the Caribbean plate and eastward migration of the Margarita Complex and its correlatives along northern South America since the Cretaceous. 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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“the lack of older blueschists may alternatively by attributed to preservation bias (Möller et al., 1995;Keller and Schoene, 2018) or that a hotter Archean mantle could have increased subduction zone geotherms outside of those required to stabilize glaucophane (Bjørnerud and Austrheim, 2004).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Möller et al., 1995
In the citing paper
“These terranes, located on the north shore of Manicouagan Reservoir, comprise the Manicouagan Imbricate zone (Indares et al. 1998, 2000), and its mapped extension into the southern part of the reservoir is described by Eaton et al. (1995) and Hynes et al. (2000).”
From The High Pressure belt in the Grenville Province: architecture, timing, and exhumation (2002) · cites this paper as Eaton et al. (1995)
In the citing paper
“Li-bearing Andean salt pans are exclusively hosted in endorheic basins (isolated hydrological units corresponding to internally drained areas).”
From Brine grades in Andean salars: When basin size matters A review of the Lithium Triangle (2021) · cites this paper as Vandervoort et al., 1995
In the citing paper
“Basement inherited heterogeneities (Hongn et al., 2007), Cenozoic Andean tectonics (actively uplifting ranges) and Neogene plateau rise were key factors for the formation of endorheic basins in the plateau, while the arid climate (Garreaud, 2009) has ensured their preservation (Vandervoort et al., 1995;López Steinmetz et al., 2020b).”
From Brine grades in Andean salars: When basin size matters A review of the Lithium Triangle (2021) · cites this paper as Vandervoort et al., 1995
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- Lallemand, S.
- Venue
- Geology
- Published
- 1995
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- Lallemand, S. (1995). High rates of arc consumption by subduction processes: Some consequences. Geology. https://doi.org/10.1130/0091-7613(1995)023%3C0551%3Ahroacb%3E2.3.co%3B2
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