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Paleomagnetic evidence of an early Paleozoic rotated terrane in Northwest Argentina; a clue for Gondwana-Laurentia interaction?
Paleomagnetic results from three Lower Ordovician units in northwest Argentina are reported. When assessed with available geologic evidence, these data permit the definition of the Puna Oriental-Famatina rotated terrane. Paleogeographic reconstructions based on these paleomagnetic results place Puna...
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Published in: | Geology (Boulder) 1996-10, Vol.24 (10), p.953-956 |
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creator | Conti, C. M Rapalini, A. E Coira, B Koukharsky, M |
description | Paleomagnetic results from three Lower Ordovician units in northwest Argentina are reported. When assessed with available geologic evidence, these data permit the definition of the Puna Oriental-Famatina rotated terrane. Paleogeographic reconstructions based on these paleomagnetic results place Puna Oriental-Famatina in the South Iapetus ocean, close to the Gondwana margin and near some of the Lower-Middle Ordovician Central Mobile belt terranes of the Northern Appalachians. The accretion of Puna Oriental-Famatina may have resulted from the closure of this ocean in Middle Ordovician time. |
doi_str_mv | 10.1130/0091-7613(1996)024<0953:PEOAEP>2.3.CO;2 |
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The accretion of Puna Oriental-Famatina may have resulted from the closure of this ocean in Middle Ordovician time.</description><subject>Argentina</subject><subject>Catamarca Argentina</subject><subject>continental drift</subject><subject>Geology</subject><subject>Gondwana</subject><subject>IGCP</subject><subject>La Rioja Argentina</subject><subject>Laurentia</subject><subject>Lower Ordovician</subject><subject>lower Paleozoic</subject><subject>Magnetism</subject><subject>Ordovician</subject><subject>paleogeography</subject><subject>paleomagnetism</subject><subject>Paleontology</subject><subject>Paleozoic</subject><subject>Puna</subject><subject>rotation</subject><subject>South America</subject><subject>Stratigraphy</subject><subject>terranes</subject><issn>0091-7613</issn><issn>1943-2682</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><recordid>eNpdkU-P0zAQxS0EEmXhO1gcEAil6z-JE7MIVFWlIFW0BzhbgzMuWaX24jhUy2W_-joEgcTB9mF-b2b8HiGXnC05l-ySMc2LWnH5kmutXjFRvmW6km8Om_1qc3gnlnK53l-JB2TBdSkLoRrxkCz-qh6TJ8NwzRgvq7pZkLsD9BhOcPSYOkvxZ9eit0iDo-ApQuxv6W_kV8jlGBIkbGnCGMEj7Tz9HGL6fsYh0VU8ok-dhysK1PYjUhci3QbfnsFDsYMxTnXIqqwHm7rg3z8ljxz0Az77816Qrx82X9Yfi91--2m92hUglErTXVpdc42V1Y1jTQOiARS1rqCqK1EqZ1vmHLals05Z3grd1Khr22oJ37S8IC_mvjcx_BjzuubUDRb7Pn8jjIMRTCuVTwaf_wdehzH6vFtmOK9Uo6oMbWfIxjAMEZ25id0J4q3hzEwpmclvM_ltppRMTslMKZk5JSOMNOu9EbnT67nTEcNgu8n7c4h9-2_qrK-bUkh5D-vlmbM</recordid><startdate>19961001</startdate><enddate>19961001</enddate><creator>Conti, C. 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M</creatorcontrib><creatorcontrib>Rapalini, A. E</creatorcontrib><creatorcontrib>Coira, B</creatorcontrib><creatorcontrib>Koukharsky, M</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geology (Boulder)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Conti, C. M</au><au>Rapalini, A. 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The accretion of Puna Oriental-Famatina may have resulted from the closure of this ocean in Middle Ordovician time.</abstract><cop>Boulder</cop><pub>Geological Society of America (GSA)</pub><doi>10.1130/0091-7613(1996)024<0953:PEOAEP>2.3.CO;2</doi><tpages>4</tpages></addata></record> |
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language | eng |
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subjects | Argentina Catamarca Argentina continental drift Geology Gondwana IGCP La Rioja Argentina Laurentia Lower Ordovician lower Paleozoic Magnetism Ordovician paleogeography paleomagnetism Paleontology Paleozoic Puna rotation South America Stratigraphy terranes |
title | Paleomagnetic evidence of an early Paleozoic rotated terrane in Northwest Argentina; a clue for Gondwana-Laurentia interaction? |
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