Reply to the comments on “Xenoliths in ultrapotassic volcanic rocks in the Lhasa block: direct evidence for crust–mantle mixing and metamorphism in the deep crust”
Stepanov et al. (Contrib Mineral Petrol, 2017 ) question our conclusion that the UPVs in southern Tibet were derived by partial melting of an old, metasomatized subcontinental lithospheric mantle (SCLM) of the subducted Indian plate. Instead, they propose that these ultrapotassic volcanic rocks (UPV...
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| creator | Wang, Rui Collins, William J. Weinberg, Roberto F. Richards, Jeremy P. He, Wen-yan |
| description | Stepanov et al. (Contrib Mineral Petrol,
2017
) question our conclusion that the UPVs in southern Tibet were derived by partial melting of an old, metasomatized subcontinental lithospheric mantle (SCLM) of the subducted Indian plate. Instead, they propose that these ultrapotassic volcanic rocks (UPVs) are shoshonitic and were generated in two steps: direct melting of crustal rocks first, and then the melts interacted with mantle peridotite. However, the trace element, isotopic, thermal, structural, and seismic evidence is consistent with the xenolith evidence (Wang et al in Contrib Mineral Petrol 172:62,
2016
) for hybridisation of ascending Indian subcontinental lithospheric mantle-derived UPV magmas with the deep, isotopically unevolved, Tibetan crust. This necessitates a model whereby partial melting of subducting Indian SCLM generates the UPV suite of southern Tibet. |
| doi_str_mv | 10.1007/s00410-017-1333-5 |
| format | Article |
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2017
) question our conclusion that the UPVs in southern Tibet were derived by partial melting of an old, metasomatized subcontinental lithospheric mantle (SCLM) of the subducted Indian plate. Instead, they propose that these ultrapotassic volcanic rocks (UPVs) are shoshonitic and were generated in two steps: direct melting of crustal rocks first, and then the melts interacted with mantle peridotite. However, the trace element, isotopic, thermal, structural, and seismic evidence is consistent with the xenolith evidence (Wang et al in Contrib Mineral Petrol 172:62,
2016
) for hybridisation of ascending Indian subcontinental lithospheric mantle-derived UPV magmas with the deep, isotopically unevolved, Tibetan crust. This necessitates a model whereby partial melting of subducting Indian SCLM generates the UPV suite of southern Tibet.</description><identifier>ISSN: 0010-7999</identifier><identifier>EISSN: 1432-0967</identifier><identifier>DOI: 10.1007/s00410-017-1333-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Direct melting ; Earth and Environmental Science ; Earth Sciences ; Geology ; Hybridization ; Mantle ; Melting ; Melts ; Metamorphism ; Metamorphism (geology) ; Mineral Resources ; Mineralogy ; Peridotite ; Petrology ; Plate tectonics ; Plates (tectonics) ; Reply ; Rocks ; Subduction (geology) ; Trace elements ; Volcanic rocks ; Volcanoes</subject><ispartof>Contributions to mineralogy and petrology, 2017-04, Vol.172 (4), p.1-5, Article 20</ispartof><rights>Springer-Verlag Berlin Heidelberg 2017</rights><rights>Contributions to Mineralogy and Petrology is a copyright of Springer, (2017). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-b2cde6798686fa2b856e96a99b1bbceb7aa98595395d5123b3adc729cec6d6313</citedby><cites>FETCH-LOGICAL-c316t-b2cde6798686fa2b856e96a99b1bbceb7aa98595395d5123b3adc729cec6d6313</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00410-017-1333-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00410-017-1333-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Wang, Rui</creatorcontrib><creatorcontrib>Collins, William J.</creatorcontrib><creatorcontrib>Weinberg, Roberto F.</creatorcontrib><creatorcontrib>Richards, Jeremy P.</creatorcontrib><creatorcontrib>He, Wen-yan</creatorcontrib><title>Reply to the comments on “Xenoliths in ultrapotassic volcanic rocks in the Lhasa block: direct evidence for crust–mantle mixing and metamorphism in the deep crust”</title><title>Contributions to mineralogy and petrology</title><addtitle>Contrib Mineral Petrol</addtitle><description>Stepanov et al. (Contrib Mineral Petrol,
2017
) question our conclusion that the UPVs in southern Tibet were derived by partial melting of an old, metasomatized subcontinental lithospheric mantle (SCLM) of the subducted Indian plate. Instead, they propose that these ultrapotassic volcanic rocks (UPVs) are shoshonitic and were generated in two steps: direct melting of crustal rocks first, and then the melts interacted with mantle peridotite. However, the trace element, isotopic, thermal, structural, and seismic evidence is consistent with the xenolith evidence (Wang et al in Contrib Mineral Petrol 172:62,
2016
) for hybridisation of ascending Indian subcontinental lithospheric mantle-derived UPV magmas with the deep, isotopically unevolved, Tibetan crust. This necessitates a model whereby partial melting of subducting Indian SCLM generates the UPV suite of southern Tibet.</description><subject>Direct melting</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Hybridization</subject><subject>Mantle</subject><subject>Melting</subject><subject>Melts</subject><subject>Metamorphism</subject><subject>Metamorphism (geology)</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Peridotite</subject><subject>Petrology</subject><subject>Plate tectonics</subject><subject>Plates (tectonics)</subject><subject>Reply</subject><subject>Rocks</subject><subject>Subduction (geology)</subject><subject>Trace elements</subject><subject>Volcanic rocks</subject><subject>Volcanoes</subject><issn>0010-7999</issn><issn>1432-0967</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kUtKBDEURYMo2H4W4CzguDSpmFTFmYg_aBBEwVlIpV7b0aqkTNJiz9yDU12A23Ilpm0FJ47e7577BhehHUr2KCHVfiTkgJKC0KqgjLGCr6ARPWBlQaSoVtGIkHytpJTraCPGe5LnWvIR-riCoZvj5HGaAja-78GliL3Dny9vt-B8Z9M0YuvwrEtBDz7pGK3BT74z2uUmePPwfV_w46mOGjdd3h3i1gYwCcOTbcEZwBMfsAmzmD5fXnvtUge4t8_W3WHtWtxD0r0Pw9TG_teuBRh-kfcttDbRXYTtn7qJbk5Pro_Pi_Hl2cXx0bgwjIpUNKVpQVSyFrWY6LKpuQAptJQNbRoDTaW1rLnkTPKW05I1TLemKqUBI1rBKNtEu0vfIfjHGcSk7v0suPxS0bomteCSlFlFlyoTfIwBJmoIttdhrihRi0TUMhGVE1GLRBTPTLlkYta6Owh_nP-FvgA-4JS8</recordid><startdate>20170401</startdate><enddate>20170401</enddate><creator>Wang, Rui</creator><creator>Collins, William J.</creator><creator>Weinberg, Roberto F.</creator><creator>Richards, Jeremy P.</creator><creator>He, Wen-yan</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KB.</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>R05</scope></search><sort><creationdate>20170401</creationdate><title>Reply to the comments on “Xenoliths in ultrapotassic volcanic rocks in the Lhasa block: direct evidence for crust–mantle mixing and metamorphism in the deep crust”</title><author>Wang, Rui ; Collins, William J. ; Weinberg, Roberto F. ; Richards, Jeremy P. ; He, Wen-yan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-b2cde6798686fa2b856e96a99b1bbceb7aa98595395d5123b3adc729cec6d6313</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Direct melting</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Hybridization</topic><topic>Mantle</topic><topic>Melting</topic><topic>Melts</topic><topic>Metamorphism</topic><topic>Metamorphism (geology)</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Peridotite</topic><topic>Petrology</topic><topic>Plate tectonics</topic><topic>Plates (tectonics)</topic><topic>Reply</topic><topic>Rocks</topic><topic>Subduction (geology)</topic><topic>Trace elements</topic><topic>Volcanic rocks</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Rui</creatorcontrib><creatorcontrib>Collins, William J.</creatorcontrib><creatorcontrib>Weinberg, Roberto F.</creatorcontrib><creatorcontrib>Richards, Jeremy P.</creatorcontrib><creatorcontrib>He, Wen-yan</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Science Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><jtitle>Contributions to mineralogy and petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Rui</au><au>Collins, William J.</au><au>Weinberg, Roberto F.</au><au>Richards, Jeremy P.</au><au>He, Wen-yan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reply to the comments on “Xenoliths in ultrapotassic volcanic rocks in the Lhasa block: direct evidence for crust–mantle mixing and metamorphism in the deep crust”</atitle><jtitle>Contributions to mineralogy and petrology</jtitle><stitle>Contrib Mineral Petrol</stitle><date>2017-04-01</date><risdate>2017</risdate><volume>172</volume><issue>4</issue><spage>1</spage><epage>5</epage><pages>1-5</pages><artnum>20</artnum><issn>0010-7999</issn><eissn>1432-0967</eissn><abstract>Stepanov et al. (Contrib Mineral Petrol,
2017
) question our conclusion that the UPVs in southern Tibet were derived by partial melting of an old, metasomatized subcontinental lithospheric mantle (SCLM) of the subducted Indian plate. Instead, they propose that these ultrapotassic volcanic rocks (UPVs) are shoshonitic and were generated in two steps: direct melting of crustal rocks first, and then the melts interacted with mantle peridotite. However, the trace element, isotopic, thermal, structural, and seismic evidence is consistent with the xenolith evidence (Wang et al in Contrib Mineral Petrol 172:62,
2016
) for hybridisation of ascending Indian subcontinental lithospheric mantle-derived UPV magmas with the deep, isotopically unevolved, Tibetan crust. This necessitates a model whereby partial melting of subducting Indian SCLM generates the UPV suite of southern Tibet.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00410-017-1333-5</doi><tpages>5</tpages></addata></record> |
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| subjects | Direct melting Earth and Environmental Science Earth Sciences Geology Hybridization Mantle Melting Melts Metamorphism Metamorphism (geology) Mineral Resources Mineralogy Peridotite Petrology Plate tectonics Plates (tectonics) Reply Rocks Subduction (geology) Trace elements Volcanic rocks Volcanoes |
| title | Reply to the comments on “Xenoliths in ultrapotassic volcanic rocks in the Lhasa block: direct evidence for crust–mantle mixing and metamorphism in the deep crust” |
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