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Mineralized fault zone parallel to the Oman ophiolite spreading axis
During the formation of the Upper Cretaceous Oman ophiolite by sea-floor spreading, faulting parallel to the spreading axis produced a 250-m escarpment. This escarpment now forms the western margin of a 5-km-wide north-south-oriented valley in northern Oman floored by pillow lavas, flow breccias, la...
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Published in: | Geology (Boulder) 1977-09, Vol.5 (9), p.534-538 |
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container_title | Geology (Boulder) |
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creator | Smewing, J. D Simonian, K. O Elboushi, I. M Gass, I. G |
description | During the formation of the Upper Cretaceous Oman ophiolite by sea-floor spreading, faulting parallel to the spreading axis produced a 250-m escarpment. This escarpment now forms the western margin of a 5-km-wide north-south-oriented valley in northern Oman floored by pillow lavas, flow breccias, laminated mudstones, and mass-flow, ophiolite-derived sediments; sulfide mineralization is concentrated along the fault zone. The features described are closely comparable with those reported in the FAMOUS area and those in a paleo-transform fault zone in the Troodos massif, Cyprus, and are significant in delineating mineralized zones in ophiolites. |
doi_str_mv | 10.1130/0091-7613(1977)5<534:MFZPTT>2.0.CO;2 |
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D ; Simonian, K. O ; Elboushi, I. M ; Gass, I. G</creator><creatorcontrib>Smewing, J. D ; Simonian, K. O ; Elboushi, I. M ; Gass, I. G</creatorcontrib><description>During the formation of the Upper Cretaceous Oman ophiolite by sea-floor spreading, faulting parallel to the spreading axis produced a 250-m escarpment. This escarpment now forms the western margin of a 5-km-wide north-south-oriented valley in northern Oman floored by pillow lavas, flow breccias, laminated mudstones, and mass-flow, ophiolite-derived sediments; sulfide mineralization is concentrated along the fault zone. The features described are closely comparable with those reported in the FAMOUS area and those in a paleo-transform fault zone in the Troodos massif, Cyprus, and are significant in delineating mineralized zones in ophiolites.</description><identifier>ISSN: 0091-7613</identifier><identifier>EISSN: 1943-2682</identifier><identifier>DOI: 10.1130/0091-7613(1977)5<534:MFZPTT>2.0.CO;2</identifier><language>eng</language><publisher>Geological Society of America (GSA)</publisher><subject>allochthons ; Arabian Peninsula ; Asia ; Cretaceous ; emplacement ; fault zones ; genesis ; Geophysics ; igneous rocks ; indicators ; Mesozoic ; mineralization ; nappes ; Oman ; ophiolite ; plate tectonics ; plutonic rocks ; sea-floor spreading ; Sohar ; solid Earth (tectonophysics) ; spreading centers ; tectonophysics ; ultramafics ; Upper Cretaceous</subject><ispartof>Geology (Boulder), 1977-09, Vol.5 (9), p.534-538</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://pubs.geoscienceworld.org/lithosphere/article-lookup?doi=10.1130/0091-7613(1977)5<534:MFZPTT>2.0.CO;2$$EHTML$$P50$$Ggeoscienceworld$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,38858,77566</link.rule.ids></links><search><creatorcontrib>Smewing, J. D</creatorcontrib><creatorcontrib>Simonian, K. O</creatorcontrib><creatorcontrib>Elboushi, I. M</creatorcontrib><creatorcontrib>Gass, I. G</creatorcontrib><title>Mineralized fault zone parallel to the Oman ophiolite spreading axis</title><title>Geology (Boulder)</title><description>During the formation of the Upper Cretaceous Oman ophiolite by sea-floor spreading, faulting parallel to the spreading axis produced a 250-m escarpment. This escarpment now forms the western margin of a 5-km-wide north-south-oriented valley in northern Oman floored by pillow lavas, flow breccias, laminated mudstones, and mass-flow, ophiolite-derived sediments; sulfide mineralization is concentrated along the fault zone. The features described are closely comparable with those reported in the FAMOUS area and those in a paleo-transform fault zone in the Troodos massif, Cyprus, and are significant in delineating mineralized zones in ophiolites.</description><subject>allochthons</subject><subject>Arabian Peninsula</subject><subject>Asia</subject><subject>Cretaceous</subject><subject>emplacement</subject><subject>fault zones</subject><subject>genesis</subject><subject>Geophysics</subject><subject>igneous rocks</subject><subject>indicators</subject><subject>Mesozoic</subject><subject>mineralization</subject><subject>nappes</subject><subject>Oman</subject><subject>ophiolite</subject><subject>plate tectonics</subject><subject>plutonic rocks</subject><subject>sea-floor spreading</subject><subject>Sohar</subject><subject>solid Earth (tectonophysics)</subject><subject>spreading centers</subject><subject>tectonophysics</subject><subject>ultramafics</subject><subject>Upper Cretaceous</subject><issn>0091-7613</issn><issn>1943-2682</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1977</creationdate><recordtype>article</recordtype><recordid>eNo9kF1r2zAYhcXoYGm2_6Cr0tE504dtSWsZlKTdBi3ZRXazGyHbrxIFxXIlh378-tq49OqFwznn5TwIfaNkQSkn3wlRNBMl5edUCfG1uCp4_uP-9v_fzeYnW5DFcn3JPqAZVTnPWCnZCZq9Rz6h05T2hNC8EHKGVveuhWi8e4EGW3P0PX4JLeDODKIHj_uA-x3g9cG0OHQ7F7zrAacugmlcu8XmyaXP6KM1PsGXtztH_25vNsvf2d3615_l9V1mOMn7jFtbSV5LOY4oGZUVLaGWtKnBWsOsqpgoLZhSUqNKXtGGC6XySklJmDCcz9HZ1NvF8HCE1OuDSzV4b1oIx6Sp4kQUhRqMq8lYx5BSBKu76A4mPmtK9Phdjzz0yEOPCHWhB4R6QqiZJnq51myouZhqthBS7aCt4TFE3-h9OMZ2WDqFSS5yQvkr0Ph2tQ</recordid><startdate>19770901</startdate><enddate>19770901</enddate><creator>Smewing, J. D</creator><creator>Simonian, K. O</creator><creator>Elboushi, I. M</creator><creator>Gass, I. G</creator><general>Geological Society of America (GSA)</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>19770901</creationdate><title>Mineralized fault zone parallel to the Oman ophiolite spreading axis</title><author>Smewing, J. D ; Simonian, K. O ; Elboushi, I. M ; Gass, I. 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D</creatorcontrib><creatorcontrib>Simonian, K. O</creatorcontrib><creatorcontrib>Elboushi, I. M</creatorcontrib><creatorcontrib>Gass, I. G</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</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>Smewing, J. D</au><au>Simonian, K. O</au><au>Elboushi, I. M</au><au>Gass, I. G</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mineralized fault zone parallel to the Oman ophiolite spreading axis</atitle><jtitle>Geology (Boulder)</jtitle><date>1977-09-01</date><risdate>1977</risdate><volume>5</volume><issue>9</issue><spage>534</spage><epage>538</epage><pages>534-538</pages><issn>0091-7613</issn><eissn>1943-2682</eissn><abstract>During the formation of the Upper Cretaceous Oman ophiolite by sea-floor spreading, faulting parallel to the spreading axis produced a 250-m escarpment. This escarpment now forms the western margin of a 5-km-wide north-south-oriented valley in northern Oman floored by pillow lavas, flow breccias, laminated mudstones, and mass-flow, ophiolite-derived sediments; sulfide mineralization is concentrated along the fault zone. The features described are closely comparable with those reported in the FAMOUS area and those in a paleo-transform fault zone in the Troodos massif, Cyprus, and are significant in delineating mineralized zones in ophiolites.</abstract><pub>Geological Society of America (GSA)</pub><doi>10.1130/0091-7613(1977)5<534:MFZPTT>2.0.CO;2</doi><tpages>5</tpages></addata></record> |
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identifier | ISSN: 0091-7613 |
ispartof | Geology (Boulder), 1977-09, Vol.5 (9), p.534-538 |
issn | 0091-7613 1943-2682 |
language | eng |
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source | GeoScienceWorld |
subjects | allochthons Arabian Peninsula Asia Cretaceous emplacement fault zones genesis Geophysics igneous rocks indicators Mesozoic mineralization nappes Oman ophiolite plate tectonics plutonic rocks sea-floor spreading Sohar solid Earth (tectonophysics) spreading centers tectonophysics ultramafics Upper Cretaceous |
title | Mineralized fault zone parallel to the Oman ophiolite spreading axis |
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