Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins
Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks ca...
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| Autor*in: |
Wang, Zhihong [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2002 |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 2002 |
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| Übergeordnetes Werk: |
Enthalten in: Contributions to mineralogy and petrology - Springer-Verlag, 1966, 143(2002), 4 vom: Juli, Seite 471-483 |
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| Übergeordnetes Werk: |
volume:143 ; year:2002 ; number:4 ; month:07 ; pages:471-483 |
| Links: |
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| DOI / URN: |
10.1007/s00410-002-0358-5 |
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| Katalog-ID: |
OLC2070521745 |
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| 245 | 1 | 0 | |a Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins |
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| 520 | |a Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. | ||
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10.1007/s00410-002-0358-5 doi (DE-627)OLC2070521745 (DE-He213)s00410-002-0358-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Wang, Zhihong verfasserin aut Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins 2002 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2002 Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. Mantle Wedge Mantle Peridotite Mantle Upwelling Deplete Mantle Source Extrusive Rock Sun, Shu aut Li, Jiliang aut Hou, Quanlin aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 143(2002), 4 vom: Juli, Seite 471-483 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:143 year:2002 number:4 month:07 pages:471-483 https://doi.org/10.1007/s00410-002-0358-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 143 2002 4 07 471-483 |
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10.1007/s00410-002-0358-5 doi (DE-627)OLC2070521745 (DE-He213)s00410-002-0358-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Wang, Zhihong verfasserin aut Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins 2002 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2002 Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. Mantle Wedge Mantle Peridotite Mantle Upwelling Deplete Mantle Source Extrusive Rock Sun, Shu aut Li, Jiliang aut Hou, Quanlin aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 143(2002), 4 vom: Juli, Seite 471-483 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:143 year:2002 number:4 month:07 pages:471-483 https://doi.org/10.1007/s00410-002-0358-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 143 2002 4 07 471-483 |
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10.1007/s00410-002-0358-5 doi (DE-627)OLC2070521745 (DE-He213)s00410-002-0358-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Wang, Zhihong verfasserin aut Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins 2002 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2002 Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. Mantle Wedge Mantle Peridotite Mantle Upwelling Deplete Mantle Source Extrusive Rock Sun, Shu aut Li, Jiliang aut Hou, Quanlin aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 143(2002), 4 vom: Juli, Seite 471-483 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:143 year:2002 number:4 month:07 pages:471-483 https://doi.org/10.1007/s00410-002-0358-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 143 2002 4 07 471-483 |
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10.1007/s00410-002-0358-5 doi (DE-627)OLC2070521745 (DE-He213)s00410-002-0358-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Wang, Zhihong verfasserin aut Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins 2002 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2002 Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. Mantle Wedge Mantle Peridotite Mantle Upwelling Deplete Mantle Source Extrusive Rock Sun, Shu aut Li, Jiliang aut Hou, Quanlin aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 143(2002), 4 vom: Juli, Seite 471-483 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:143 year:2002 number:4 month:07 pages:471-483 https://doi.org/10.1007/s00410-002-0358-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 143 2002 4 07 471-483 |
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10.1007/s00410-002-0358-5 doi (DE-627)OLC2070521745 (DE-He213)s00410-002-0358-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Wang, Zhihong verfasserin aut Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins 2002 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2002 Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. Mantle Wedge Mantle Peridotite Mantle Upwelling Deplete Mantle Source Extrusive Rock Sun, Shu aut Li, Jiliang aut Hou, Quanlin aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 143(2002), 4 vom: Juli, Seite 471-483 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:143 year:2002 number:4 month:07 pages:471-483 https://doi.org/10.1007/s00410-002-0358-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 143 2002 4 07 471-483 |
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The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. 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petrogenesis of tholeiite associations in kudi ophiolite (western kunlun mountains, northwestern china): implications for the evolution of back-arc basins |
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Petrogenesis of tholeiite associations in Kudi ophiolite (western Kunlun Mountains, northwestern China): implications for the evolution of back-arc basins |
| abstract |
Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. © Springer-Verlag 2002 |
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Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. © Springer-Verlag 2002 |
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Abstract. The Kudi ophiolite in the western Kunlun Mountains comprises harzburgites, dunites, cumulate dunites, cumulate pyroxenites and gabbros, diabase dikes, and pillow and massive lavas, and are fragments of a supra-subduction zone (SSZ) ophiolite from the Early Paleozoic. The extrusive rocks can be classified into three groups of tholeiites: back-arc basin (BAB) tholeiites, low-Ti island arc tholeiites (IAT), and LREE-enriched IAT, as shown by their distinctive geochemical characteristics. The SSZ-type mantle peridotites, the cumulate complex with arc tholeiite affinity, and BABB-type diabase dikes and basalts constitute an upper mantle and crustal section of a back-arc basin formed by coupling of MORB-type mantle upwelling with fluid efflux from slab devolatilization. The low-Ti IAT are characterized by low Ti and HFSE, and slightly U-shaped or LREE-depleted chondrite-normalized REE patterns, and represent melts derived from a depleted mantle source region (extraction of BABB magma) modified compositionally by fluids and/or melts from the subducting lithospheric slab during propagation and extension of the back-arc basin. We interpret the LREE-enriched IAT as products of closure of the back-arc basin because an interaction between the parental magma of this IAT and the mantle peridotites (formerly the upper mantle of the basin) in a newly formed mantle wedge had occurred. © Springer-Verlag 2002 |
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