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Controls of Stratigraphic Architecture on Along Strike Cooling Age Patterns
Cooling related to moving rocks over an ~8.5 km vertically thick ramp in the Main Himalayan thrust (MHT) produced 0.8–2 Ma zircon (U–Th)/He (ZHe) and apatite fission track (AFT) ages from the Main Central thrust to 40 km south in central Nepal. The ramp size is controlled by thicker Proterozoic stra...
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Published in: | Terra nova (Oxford, England) England), 2021-04, Vol.33 (2), p.129-136 |
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creator | Robinson, Delores M. Khanal, Subodha Olree, Elizabeth Bhattacharya, Gourab Mandal, Subhadip |
description | Cooling related to moving rocks over an ~8.5 km vertically thick ramp in the Main Himalayan thrust (MHT) produced 0.8–2 Ma zircon (U–Th)/He (ZHe) and apatite fission track (AFT) ages from the Main Central thrust to 40 km south in central Nepal. The ramp size is controlled by thicker Proterozoic stratigraphy. ZHe ages in NW India and eastern Bhutan over a similar 40 km wide swath are 1.4–12 Ma. In addition, the ZHe ages are consistently 2–5 million years older than the AFT ages. We argue that the MHT ramps are smaller because of thinner Proterozoic stratigraphy, with two vertically thick ramps of 2.5 km each in eastern Bhutan and one vertically thick ramp of ~5 km in NW India. Thus, the original stratigraphy and associated weaker décollement horizons control location and size of active MHT ramps, resulting vertical uplift, and along strike pattern of cooling ages. |
doi_str_mv | 10.1111/ter.12498 |
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The ramp size is controlled by thicker Proterozoic stratigraphy. ZHe ages in NW India and eastern Bhutan over a similar 40 km wide swath are 1.4–12 Ma. In addition, the ZHe ages are consistently 2–5 million years older than the AFT ages. We argue that the MHT ramps are smaller because of thinner Proterozoic stratigraphy, with two vertically thick ramps of 2.5 km each in eastern Bhutan and one vertically thick ramp of ~5 km in NW India. 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Thus, the original stratigraphy and associated weaker décollement horizons control location and size of active MHT ramps, resulting vertical uplift, and along strike pattern of cooling ages.</description><subject>Apatite</subject><subject>Cooling</subject><subject>Himalaya</subject><subject>Lesser Himalaya</subject><subject>Main Himalayan thrust</subject><subject>Precambrian</subject><subject>ramps</subject><subject>Stratigraphy</subject><subject>thermochonology</subject><subject>Uplift</subject><subject>Zircon</subject><issn>0954-4879</issn><issn>1365-3121</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kM1OwzAQhC0EEqVw4A0sceKQdmM7cXyMovIjKoGgnK1N6rQpIS62I9S3JyVc2ctopW9nVkPIdQyzeJh5MG4WM6GyEzKJeZpEPGbxKZmASkQkMqnOyYX3OwCQkqkJeSpsF5xtPbU1fQsOQ7NxuN82Fc1dtW2CqULvDLUdzVvbbY5M82FoYW3bDGu-MfQFwxDb-UtyVmPrzdWfTsn73WJVPETL5_vHIl9GFecsiziiKFEksgRIVbZOalbWSoDKkEGiUszWmEo0EoVZVwBlwiViprCWLAVT8ym5GX33zn71xge9s73rhkjNEgCeSiXUQN2OVOWs987Ueu-aT3QHHYM-dqWHp_VvVwM7H9nvpjWH_0G9WryOFz_tF2rn</recordid><startdate>202104</startdate><enddate>202104</enddate><creator>Robinson, Delores M.</creator><creator>Khanal, Subodha</creator><creator>Olree, Elizabeth</creator><creator>Bhattacharya, Gourab</creator><creator>Mandal, Subhadip</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-5828-7361</orcidid><orcidid>https://orcid.org/0000-0002-7618-7209</orcidid></search><sort><creationdate>202104</creationdate><title>Controls of Stratigraphic Architecture on Along Strike Cooling Age Patterns</title><author>Robinson, Delores M. ; Khanal, Subodha ; Olree, Elizabeth ; Bhattacharya, Gourab ; Mandal, Subhadip</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3328-3aa4ba457b00698d5f2bf94098a20596a8da67ae7a4edc00b537aa89af7260ef3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Apatite</topic><topic>Cooling</topic><topic>Himalaya</topic><topic>Lesser Himalaya</topic><topic>Main Himalayan thrust</topic><topic>Precambrian</topic><topic>ramps</topic><topic>Stratigraphy</topic><topic>thermochonology</topic><topic>Uplift</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Robinson, Delores M.</creatorcontrib><creatorcontrib>Khanal, Subodha</creatorcontrib><creatorcontrib>Olree, Elizabeth</creatorcontrib><creatorcontrib>Bhattacharya, Gourab</creatorcontrib><creatorcontrib>Mandal, Subhadip</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>Terra nova (Oxford, England)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Robinson, Delores M.</au><au>Khanal, Subodha</au><au>Olree, Elizabeth</au><au>Bhattacharya, Gourab</au><au>Mandal, Subhadip</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Controls of Stratigraphic Architecture on Along Strike Cooling Age Patterns</atitle><jtitle>Terra nova (Oxford, England)</jtitle><date>2021-04</date><risdate>2021</risdate><volume>33</volume><issue>2</issue><spage>129</spage><epage>136</epage><pages>129-136</pages><issn>0954-4879</issn><eissn>1365-3121</eissn><abstract>Cooling related to moving rocks over an ~8.5 km vertically thick ramp in the Main Himalayan thrust (MHT) produced 0.8–2 Ma zircon (U–Th)/He (ZHe) and apatite fission track (AFT) ages from the Main Central thrust to 40 km south in central Nepal. The ramp size is controlled by thicker Proterozoic stratigraphy. ZHe ages in NW India and eastern Bhutan over a similar 40 km wide swath are 1.4–12 Ma. In addition, the ZHe ages are consistently 2–5 million years older than the AFT ages. We argue that the MHT ramps are smaller because of thinner Proterozoic stratigraphy, with two vertically thick ramps of 2.5 km each in eastern Bhutan and one vertically thick ramp of ~5 km in NW India. Thus, the original stratigraphy and associated weaker décollement horizons control location and size of active MHT ramps, resulting vertical uplift, and along strike pattern of cooling ages.</abstract><cop>Oxford</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/ter.12498</doi><tpages>8</tpages><orcidid>https://orcid.org/0000-0002-5828-7361</orcidid><orcidid>https://orcid.org/0000-0002-7618-7209</orcidid><oa>free_for_read</oa></addata></record> |
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source | Wiley |
subjects | Apatite Cooling Himalaya Lesser Himalaya Main Himalayan thrust Precambrian ramps Stratigraphy thermochonology Uplift Zircon |
title | Controls of Stratigraphic Architecture on Along Strike Cooling Age Patterns |
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