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Permian Emeishan Mantle

The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP).

High-temperature melting of different crustal levels in the inner zone of the Emeishan large igneous province: Constraints from the Permian ferrosyenite and granite from the Panxi region

Permian Emeishan Mantle

The provenance of the anomalous natural gamma-ray deposition mainly includes weathering basalts and syndepositional falling acidic volcanic ash, wherein the abnormally high radioactive elements contents (Th, U) are attributed to acidic volcanic ash deposition during the Late Permian Emeishan mantle plume activity.

Distribution of Radioactive Elements (Th, U) and Formation Mechanism of the Bottom of the Lopingian (Late Permian) coal-bearing series in western Guizhou, SW China

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emeishan mantle plume

The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP).

High-temperature melting of different crustal levels in the inner zone of the Emeishan large igneous province: Constraints from the Permian ferrosyenite and granite from the Panxi region

emeishan mantle plume

Magma-carbonate interaction and recycled oceanic crust in the mantle source are thought to have played a critical role in the genesis of magmatic Fe-Ti-V oxide ore deposits in the Emeishan mantle plume-related large igneous province in southwestern China.

Sr-Nd-Hf-O isotope constraints on crustal contamination and mantle source variation of three Fe-Ti-V oxide ore deposits in the Emeishan large igneous province

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10.1016/J.LITHOS.2021.105979

The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP).

High-temperature melting of different crustal levels in the inner zone of the Emeishan large igneous province: Constraints from the Permian ferrosyenite and granite from the Panxi region

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10.1016/j.gca.2020.10.006

Magma-carbonate interaction and recycled oceanic crust in the mantle source are thought to have played a critical role in the genesis of magmatic Fe-Ti-V oxide ore deposits in the Emeishan mantle plume-related large igneous province in southwestern China.

Sr-Nd-Hf-O isotope constraints on crustal contamination and mantle source variation of three Fe-Ti-V oxide ore deposits in the Emeishan large igneous province

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10.1016/J.MARPETGEO.2021.105226

The Emeishan mantle plume is supposed to play an important role in the Permian thermal regime and source rock hydrocarbon generation evolution in the Sichuan Basin, Southwest China.

Permian geothermal units in the Sichuan Basin: Implications for the thermal effect of the Emeishan mantle plume

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10.1016/J.PETROL.2021.108779

The provenance of the anomalous natural gamma-ray deposition mainly includes weathering basalts and syndepositional falling acidic volcanic ash, wherein the abnormally high radioactive elements contents (Th, U) are attributed to acidic volcanic ash deposition during the Late Permian Emeishan mantle plume activity.

Distribution of Radioactive Elements (Th, U) and Formation Mechanism of the Bottom of the Lopingian (Late Permian) coal-bearing series in western Guizhou, SW China

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10.1016/j.oregeorev.2021.104450

The basalts in the study area formed in the shallow part of the Emeishan mantle plume by low degree of assimilation-contamination in intraplate environment.

Genesis of the Xiaotongchang basalt-hosted copper deposit in the Jinping area, SW China: Constraints from geochronology, fluid inclusion and geochemistry

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10.1016/J.LITHOS.2021.105994

The link of the widespread Late Permian–Triassic magmatism in the southwestern corner of the South China block to a subduction zone or the Emeishan mantle plume is debated.

Late Permian–Early Triassic mafic dikes in the southwestern margin of the South China block: Evidence for Paleo-Pacific subduction

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10.1017/s0016756818000493

250 Ma mafic magmatism in this area was probably related to post-flood-basalt extension associated with the Emeishan mantle plume or rollback of the subducting Palaeo-Tethys slab.

Geochronology of Early Mesozoic Diabase Units in Southwestern China: Metallogenic and Tectonic Implications

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10.1016/J.LITHOS.2019.105160

Contemporaneous alkaline and gabbroic intrusions are commonly observed around high-Ti basalt in the inner zone of Emeishan large igneous province (ELIP), the distribution and origin of these igneous rocks are significant to understand the process associated with a head of Emeishan mantle plume activity.

Origin of Late Permian syenite and gabbro from the Panxi rift, SW China: The fractionation process of mafic magma in the inner zone of the Emeishan mantle plume

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10.1016/j.ngib.2019.02.002

The following research results were obtained: (1) the Permian volcanic rocks in western Sichuan Basin are well developed and its tectonic setting is consistent with that of Emeishan basalt, which is the product of the Emeishan mantle plume.

Characteristics of Permian volcanism in the western Sichuan Basin and its natural gas exploration potential

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Emeishan Mantle
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What is/are Emeishan Mantle?

Emeishan Mantle - The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP). [1] Magma-carbonate interaction and recycled oceanic crust in the mantle source are thought to have played a critical role in the genesis of magmatic Fe-Ti-V oxide ore deposits in the Emeishan mantle plume-related large igneous province in southwestern China. [2] The Emeishan mantle plume is supposed to play an important role in the Permian thermal regime and source rock hydrocarbon generation evolution in the Sichuan Basin, Southwest China. [3] The provenance of the anomalous natural gamma-ray deposition mainly includes weathering basalts and syndepositional falling acidic volcanic ash, wherein the abnormally high radioactive elements contents (Th, U) are attributed to acidic volcanic ash deposition during the Late Permian Emeishan mantle plume activity. [4] The basalts in the study area formed in the shallow part of the Emeishan mantle plume by low degree of assimilation-contamination in intraplate environment. [5] The link of the widespread Late Permian–Triassic magmatism in the southwestern corner of the South China block to a subduction zone or the Emeishan mantle plume is debated. [6] 250 Ma mafic magmatism in this area was probably related to post-flood-basalt extension associated with the Emeishan mantle plume or rollback of the subducting Palaeo-Tethys slab. [7] Contemporaneous alkaline and gabbroic intrusions are commonly observed around high-Ti basalt in the inner zone of Emeishan large igneous province (ELIP), the distribution and origin of these igneous rocks are significant to understand the process associated with a head of Emeishan mantle plume activity. [8] The following research results were obtained: (1) the Permian volcanic rocks in western Sichuan Basin are well developed and its tectonic setting is consistent with that of Emeishan basalt, which is the product of the Emeishan mantle plume. [9]

Permian Emeishan Mantle

The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP). [1] The provenance of the anomalous natural gamma-ray deposition mainly includes weathering basalts and syndepositional falling acidic volcanic ash, wherein the abnormally high radioactive elements contents (Th, U) are attributed to acidic volcanic ash deposition during the Late Permian Emeishan mantle plume activity. [2]

emeishan mantle plume

The Late-Permian Emeishan mantle plume event caused large-scale flood basalts and related mafic-ultramafic layered mafic intrusions in the inner zone of the Emeishan large igneous province (ELIP). [1] Magma-carbonate interaction and recycled oceanic crust in the mantle source are thought to have played a critical role in the genesis of magmatic Fe-Ti-V oxide ore deposits in the Emeishan mantle plume-related large igneous province in southwestern China. [2] The Emeishan mantle plume is supposed to play an important role in the Permian thermal regime and source rock hydrocarbon generation evolution in the Sichuan Basin, Southwest China. [3] The provenance of the anomalous natural gamma-ray deposition mainly includes weathering basalts and syndepositional falling acidic volcanic ash, wherein the abnormally high radioactive elements contents (Th, U) are attributed to acidic volcanic ash deposition during the Late Permian Emeishan mantle plume activity. [4] The basalts in the study area formed in the shallow part of the Emeishan mantle plume by low degree of assimilation-contamination in intraplate environment. [5] The link of the widespread Late Permian–Triassic magmatism in the southwestern corner of the South China block to a subduction zone or the Emeishan mantle plume is debated. [6] 250 Ma mafic magmatism in this area was probably related to post-flood-basalt extension associated with the Emeishan mantle plume or rollback of the subducting Palaeo-Tethys slab. [7] Contemporaneous alkaline and gabbroic intrusions are commonly observed around high-Ti basalt in the inner zone of Emeishan large igneous province (ELIP), the distribution and origin of these igneous rocks are significant to understand the process associated with a head of Emeishan mantle plume activity. [8] The following research results were obtained: (1) the Permian volcanic rocks in western Sichuan Basin are well developed and its tectonic setting is consistent with that of Emeishan basalt, which is the product of the Emeishan mantle plume. [9]