A cumulate syenite in the upper part of the Hongge-layered mafic–ultramafic intrusion, Emeishan large igneous province, SW China

Many silicic plutonic rocks of the Late Permian Emeishan large igneous province (ELIP) are spatially and temporally related to oxide ore-bearing layered mafic–ultramafic intrusions. Their association suggests that there may be a petrogenetic link between the two rock types where the layered intrusio...

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Published in	International journal of earth sciences : Geologische Rundschau Vol. 110; no. 8; pp. 2979 - 3000
Main Author	Shellnutt, J. Gregory
Format	Journal Article
Language	English
Published	Berlin/Heidelberg Springer Berlin Heidelberg 01.11.2021 Springer Nature B.V
Subjects	Contamination Earth and Environmental Science Earth Sciences Feldspars Gabbros Geochemistry Geology Geophysics/Geodesy Intrusion Isotopes Lava Magma Mineral Resources Original Paper Permian Plagioclase Radiometric dating Rhyolite Rhyolites Rock Rocks Sedimentology Strontium 87 Strontium isotopes Structural Geology Syenite Zircon Hongge-layered intrusion Petrological modeling Metaluminous syenite Late Permian Emeishan large igneous province
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Abstract	Many silicic plutonic rocks of the Late Permian Emeishan large igneous province (ELIP) are spatially and temporally related to oxide ore-bearing layered mafic–ultramafic intrusions. Their association suggests that there may be a petrogenetic link between the two rock types where the layered intrusion represents the cumulate portion of the magma system and the silicic rocks are the residual liquid portion. An alkali feldspar syenite collected in close spatial association with the Hongge-layered mafic–ultramafic intrusion yielded a weighted-mean zircon U–Pb age of 261.5 ± 2.4 Ma with a corresponding weighted-mean ε Hf ( t ) value of + 6.5 ± 0.5. The Hongge syenite is alkalic, metaluminous, and ferroan and somewhat similar to other A-type granitoids of the ELIP but, it is composed of ~ 90 vol% alkali feldspar. The rocks have initial 87 Sr/ 86 Sr ratios of 0.70570 and 0.70515 and ε Nd ( t ) values of − 0.3 and + 1.4. Rhyolite-MELTS and isotopic modeling indicate that the Hongge syenite is likely produced by crystal accumulation of a residual silicic liquid derived from a mafic parental magma that experienced localized crustal contamination during emplacement. Moreover, the age, location, and composition of the Hongge syenite suggests that it is the uppermost portion of the Hongge-layered intrusion and is representative of the residual silicic liquid of the mafic magmas that form the plagioclase-rich cumulate gabbros of the upper zone.
AbstractList	Many silicic plutonic rocks of the Late Permian Emeishan large igneous province (ELIP) are spatially and temporally related to oxide ore-bearing layered mafic–ultramafic intrusions. Their association suggests that there may be a petrogenetic link between the two rock types where the layered intrusion represents the cumulate portion of the magma system and the silicic rocks are the residual liquid portion. An alkali feldspar syenite collected in close spatial association with the Hongge-layered mafic–ultramafic intrusion yielded a weighted-mean zircon U–Pb age of 261.5 ± 2.4 Ma with a corresponding weighted-mean ε Hf ( t ) value of + 6.5 ± 0.5. The Hongge syenite is alkalic, metaluminous, and ferroan and somewhat similar to other A-type granitoids of the ELIP but, it is composed of ~ 90 vol% alkali feldspar. The rocks have initial 87 Sr/ 86 Sr ratios of 0.70570 and 0.70515 and ε Nd ( t ) values of − 0.3 and + 1.4. Rhyolite-MELTS and isotopic modeling indicate that the Hongge syenite is likely produced by crystal accumulation of a residual silicic liquid derived from a mafic parental magma that experienced localized crustal contamination during emplacement. Moreover, the age, location, and composition of the Hongge syenite suggests that it is the uppermost portion of the Hongge-layered intrusion and is representative of the residual silicic liquid of the mafic magmas that form the plagioclase-rich cumulate gabbros of the upper zone. Many silicic plutonic rocks of the Late Permian Emeishan large igneous province (ELIP) are spatially and temporally related to oxide ore-bearing layered mafic–ultramafic intrusions. Their association suggests that there may be a petrogenetic link between the two rock types where the layered intrusion represents the cumulate portion of the magma system and the silicic rocks are the residual liquid portion. An alkali feldspar syenite collected in close spatial association with the Hongge-layered mafic–ultramafic intrusion yielded a weighted-mean zircon U–Pb age of 261.5 ± 2.4 Ma with a corresponding weighted-mean εHf(t) value of + 6.5 ± 0.5. The Hongge syenite is alkalic, metaluminous, and ferroan and somewhat similar to other A-type granitoids of the ELIP but, it is composed of ~ 90 vol% alkali feldspar. The rocks have initial 87Sr/86Sr ratios of 0.70570 and 0.70515 and εNd(t) values of − 0.3 and + 1.4. Rhyolite-MELTS and isotopic modeling indicate that the Hongge syenite is likely produced by crystal accumulation of a residual silicic liquid derived from a mafic parental magma that experienced localized crustal contamination during emplacement. Moreover, the age, location, and composition of the Hongge syenite suggests that it is the uppermost portion of the Hongge-layered intrusion and is representative of the residual silicic liquid of the mafic magmas that form the plagioclase-rich cumulate gabbros of the upper zone.
Author	Shellnutt, J. Gregory
Author_xml	– sequence: 1 givenname: J. Gregory orcidid: 0000-0003-2289-2903 surname: Shellnutt fullname: Shellnutt, J. Gregory email: jgshelln@ntnu.edu.tw organization: Department of Earth Sciences, National Taiwan Normal University
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CitedBy_id	crossref_primary_10_1016_j_lithos_2024_107932 crossref_primary_10_1016_j_lithos_2024_107724 crossref_primary_10_2475_001c_94773 crossref_primary_10_3390_min15020190 crossref_primary_10_1144_jgs2024_017 crossref_primary_10_1016_j_lithos_2022_106844 crossref_primary_10_1016_j_jseaes_2023_105893 crossref_primary_10_1007_s11631_024_00731_0 crossref_primary_10_1016_j_chemgeo_2023_121423
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Keywords	Hongge-layered intrusion Petrological modeling Metaluminous syenite Late Permian Emeishan large igneous province
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Snippet	Many silicic plutonic rocks of the Late Permian Emeishan large igneous province (ELIP) are spatially and temporally related to oxide ore-bearing layered...
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SubjectTerms	Contamination Earth and Environmental Science Earth Sciences Feldspars Gabbros Geochemistry Geology Geophysics/Geodesy Intrusion Isotopes Lava Magma Mineral Resources Original Paper Permian Plagioclase Radiometric dating Rhyolite Rhyolites Rock Rocks Sedimentology Strontium 87 Strontium isotopes Structural Geology Syenite Zircon
Title	A cumulate syenite in the upper part of the Hongge-layered mafic–ultramafic intrusion, Emeishan large igneous province, SW China
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