No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China
The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits form...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhu, Bei [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Umfang: |
11 |
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| Übergeordnetes Werk: |
Enthalten in: Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications - Piccino, Sébastien ELSEVIER, 2014transfer abstract, an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:269 ; year:2014 ; day:1 ; month:01 ; pages:57-67 ; extent:11 |
| Links: |
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| DOI / URN: |
10.1016/j.jvolgeores.2013.11.015 |
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ELV028141407 |
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| 520 | |a The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. | ||
| 520 | |a The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. | ||
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| 700 | 1 | |a Liu, Runchao |4 oth | |
| 700 | 1 | |a Liu, Dongdong |4 oth | |
| 700 | 1 | |a Du, Wei |4 oth | |
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10.1016/j.jvolgeores.2013.11.015 doi GBVA2014012000018.pica (DE-627)ELV028141407 (ELSEVIER)S0377-0273(13)00351-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 630 VZ 640 VZ 540 VZ 660 VZ 340 330 VZ 2 ssgn INTRECHT DE-1a fid 83.00 bkl Zhu, Bei verfasserin aut No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. Guo, Zhaojie oth Liu, Runchao oth Liu, Dongdong oth Du, Wei oth Enthalten in Elsevier Science Piccino, Sébastien ELSEVIER Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications 2014transfer abstract an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research Amsterdam [u.a.] (DE-627)ELV017774535 volume:269 year:2014 day:1 month:01 pages:57-67 extent:11 https://doi.org/10.1016/j.jvolgeores.2013.11.015 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-INTRECHT GBV_ILN_70 83.00 Volkswirtschaft: Allgemeines VZ AR 269 2014 1 0101 57-67 11 045F 550 |
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10.1016/j.jvolgeores.2013.11.015 doi GBVA2014012000018.pica (DE-627)ELV028141407 (ELSEVIER)S0377-0273(13)00351-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 630 VZ 640 VZ 540 VZ 660 VZ 340 330 VZ 2 ssgn INTRECHT DE-1a fid 83.00 bkl Zhu, Bei verfasserin aut No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. Guo, Zhaojie oth Liu, Runchao oth Liu, Dongdong oth Du, Wei oth Enthalten in Elsevier Science Piccino, Sébastien ELSEVIER Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications 2014transfer abstract an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research Amsterdam [u.a.] (DE-627)ELV017774535 volume:269 year:2014 day:1 month:01 pages:57-67 extent:11 https://doi.org/10.1016/j.jvolgeores.2013.11.015 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-INTRECHT GBV_ILN_70 83.00 Volkswirtschaft: Allgemeines VZ AR 269 2014 1 0101 57-67 11 045F 550 |
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10.1016/j.jvolgeores.2013.11.015 doi GBVA2014012000018.pica (DE-627)ELV028141407 (ELSEVIER)S0377-0273(13)00351-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 630 VZ 640 VZ 540 VZ 660 VZ 340 330 VZ 2 ssgn INTRECHT DE-1a fid 83.00 bkl Zhu, Bei verfasserin aut No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. Guo, Zhaojie oth Liu, Runchao oth Liu, Dongdong oth Du, Wei oth Enthalten in Elsevier Science Piccino, Sébastien ELSEVIER Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications 2014transfer abstract an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research Amsterdam [u.a.] (DE-627)ELV017774535 volume:269 year:2014 day:1 month:01 pages:57-67 extent:11 https://doi.org/10.1016/j.jvolgeores.2013.11.015 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-INTRECHT GBV_ILN_70 83.00 Volkswirtschaft: Allgemeines VZ AR 269 2014 1 0101 57-67 11 045F 550 |
| allfieldsGer |
10.1016/j.jvolgeores.2013.11.015 doi GBVA2014012000018.pica (DE-627)ELV028141407 (ELSEVIER)S0377-0273(13)00351-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 630 VZ 640 VZ 540 VZ 660 VZ 340 330 VZ 2 ssgn INTRECHT DE-1a fid 83.00 bkl Zhu, Bei verfasserin aut No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. Guo, Zhaojie oth Liu, Runchao oth Liu, Dongdong oth Du, Wei oth Enthalten in Elsevier Science Piccino, Sébastien ELSEVIER Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications 2014transfer abstract an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research Amsterdam [u.a.] (DE-627)ELV017774535 volume:269 year:2014 day:1 month:01 pages:57-67 extent:11 https://doi.org/10.1016/j.jvolgeores.2013.11.015 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-INTRECHT GBV_ILN_70 83.00 Volkswirtschaft: Allgemeines VZ AR 269 2014 1 0101 57-67 11 045F 550 |
| allfieldsSound |
10.1016/j.jvolgeores.2013.11.015 doi GBVA2014012000018.pica (DE-627)ELV028141407 (ELSEVIER)S0377-0273(13)00351-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 630 VZ 640 VZ 540 VZ 660 VZ 340 330 VZ 2 ssgn INTRECHT DE-1a fid 83.00 bkl Zhu, Bei verfasserin aut No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China 2014transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. 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No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China |
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The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. |
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The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. |
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The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV028141407</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625153257.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2014 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jvolgeores.2013.11.015</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBVA2014012000018.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV028141407</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0377-0273(13)00351-X</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">630</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">640</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">660</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">340</subfield><subfield code="a">330</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">2</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">INTRECHT</subfield><subfield code="q">DE-1a</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">83.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Bei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">No pre-eruptive uplift in the Emeishan large igneous province: New evidences from its ‘inner zone’, Dali area, Southwest China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2014transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">11</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Permian Emeishan large igneous province (ELIP) in Southwest China has been considered a typical example of crustal domal uplift caused by mantle plume upwelling prior to the onset of volcanism. However, this model has been questioned by the discovery of hydromagmatic volcaniclastic deposits formed in a marine environment, located near the central ELIP area (the ‘inner zone’) which is inferred to be the zone of maximum uplift. The volcanology of the inner zone has thus far been poorly documented, fueling the debate about whether or not pre-eruptive uplift occurred prior to plume upwelling. Understanding the volcanology of this inner zone is therefore critical in constraining the eruption environment of the central ELIP. Our work has revealed new volcanological observations in the inner zone (Dali area), which can systematically constrain volcanism and paleoenvironment. The Basal Succession of the sequence is a thick pillow lavas pile with hyaloclastites, implying an initial deeper submarine stage of eruptions. Limestones and submarine fallout tuffs are interbedded with these pillow lavas. Above that, abundant mafic volcaniclastic products developed, which contain palagonite-rimmed lapilli-tuffs, base surge deposits and peperites, suggesting hydroclastic volcanism in a shallower submarine environment. The Upper Succession of the sequence preserves columnar-jointed lava flows and subaerial fallout tuffs, reflecting subaerial volcanism after the volcanic center emerged above the sea level. These abundant and systematic natures of this evidence suggest that the initial volcanism of the central ELIP occurred in a deep submarine environment. The submarine-to-subaerial transition is caused by progressive emplacement of voluminous magmatic products infilling the inner zone during the continuous emplacement of ELIP, rather than by crustal doming prior to the onset of volcanisms.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Guo, Zhaojie</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Runchao</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Dongdong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Du, Wei</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Piccino, Sébastien ELSEVIER</subfield><subfield code="t">Aromatic composition and potent odorants of the “specialty coffee” brew “Bourbon Pointu” correlated to its three trade classifications</subfield><subfield code="d">2014transfer abstract</subfield><subfield code="d">an international journal on the geophysical, geochemical, petrological, economic and environmental aspects of volcanology and geothermal research</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV017774535</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:269</subfield><subfield code="g">year:2014</subfield><subfield code="g">day:1</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:57-67</subfield><subfield code="g">extent:11</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jvolgeores.2013.11.015</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-INTRECHT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">83.00</subfield><subfield code="j">Volkswirtschaft: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">269</subfield><subfield code="j">2014</subfield><subfield code="b">1</subfield><subfield code="c">0101</subfield><subfield code="h">57-67</subfield><subfield code="g">11</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
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