Rift- and subduction-related crustal sequences in the Jinshajiang ophiolitic melange, SW China; insights into the eastern Paleo-Tethys

The Paleozoic Jinshajiang ophiolitic melange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys. Basic-intermediate rocks are widespread features in the melange; their formation age is well known, but the petrogenesis has not been well studied, which...

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Published inLithosphere Vol. 11; no. 6; pp. 821 - 833
Main Authors Hu Wenjun, Hu Wenjun, Zhong Hong, Zhong Hong, Zhu Weiguang, Zhu Weiguang, Bai Zhongjie, Bai Zhongjie
Format Journal Article
LanguageEnglish
Published Geological Society of America 01.12.2019
Subjects
Ailao Shan
Ailaoshan Ophiolite
Ailaoshan suture zone
alkaline earth metals
Asia
Baimaxueshan
basalts
Benzilan China
Changning-Menglian Ophiolite
China
crust
diabase
Far East
gabbros
Geochemistry
Geophysics
harzburgite
ICP mass spectra
igneous rocks
isotope ratios
isotopes
Jianshajiang suture zone
Jinshajiang Ocean
Jinshajiang ophiolitic melange
Jinshajiang-Ailaoshan Ocean
lanthanum
lava
lithosphere
major elements
mass spectra
melange
metals
metamorphism
metasomatism
mid-ocean ridge basalts
Nd-144/Nd-143
neodymium
niobium
ophiolite
paleo-oceanography
paleogeography
Paleotethys
peridotites
plate tectonics
plutonic rocks
radioactive isotopes
rare earths
rifting
samarium
Sanjiang
sea-floor spreading
serpentinization
Sibumasu China
Sichuan China
Sm-147/Nd-144
solid Earth (tectonophysics)
southwestern China
spectra
Sr-87/Sr-86
stable isotopes
strontium
subduction
suture zones
trace elements
ultramafics
volcanic rocks
whole rock
X-ray fluorescence spectra
Yunnan China
Zhiyong China
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Abstract The Paleozoic Jinshajiang ophiolitic melange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys. Basic-intermediate rocks are widespread features in the melange; their formation age is well known, but the petrogenesis has not been well studied, which means that the evolutionary history of the Jinshajiang Ocean is not well constrained. To understand the nature of the melange and the ocean, we present a set of elemental and isotopic data from two typical crustal sequences in two areas of the Jinshajiang ophiolitic melange, Zhiyong and Baimaxueshan. The basalts in the ca. 343 Ma Zhiyong crustal sequence show mid-ocean-ridge basalt-like geochemical compositions with Nb/La ratios of 0.98-1.15 and εNd(t) values of +6.5 to +7.7, indicating that the basalts formed in the spreading ridge of the ocean. In contrast, the 283 Ma Baimaxueshan crustal sequence consists of gabbros and basaltic-andesitic lavas, which have an arc affinity with Nb/La ratios of 0.54-0.67 and εNd(t) values of +5.1 to +6.5. The geochemical differences were not caused by crustal assimilation but reflect mantle metasomatism by fluids dehydrated from the subducting slab. Therefore, we propose that the Zhiyong and Baimaxueshan crustal sequences formed in seafloor spreading and subduction settings, which were related to the opening and closure of the ocean, respectively.
AbstractList Abstract The Paleozoic Jinshajiang ophiolitic mélange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys. Basic-intermediate rocks are widespread features in the mélange; their formation age is well known, but the petrogenesis has not been well studied, which means that the evolutionary history of the Jinshajiang Ocean is not well constrained. To understand the nature of the mélange and the ocean, we present a set of elemental and isotopic data from two typical crustal sequences in two areas of the Jinshajiang ophiolitic mélange, Zhiyong and Baimaxueshan. The basalts in the ca. 343 Ma Zhiyong crustal sequence show mid-ocean-ridge basalt–like geochemical compositions with Nb/La ratios of 0.98–1.15 and εNd(t) values of +6.5 to +7.7, indicating that the basalts formed in the spreading ridge of the ocean. In contrast, the 283 Ma Baimaxueshan crustal sequence consists of gabbros and basaltic-andesitic lavas, which have an arc affinity with Nb/La ratios of 0.54–0.67 and εNd(t) values of +5.1 to +6.5. The geochemical differences were not caused by crustal assimilation but reflect mantle metasomatism by fluids dehydrated from the subducting slab. Therefore, we propose that the Zhiyong and Baimaxueshan crustal sequences formed in seafloor spreading and subduction settings, which were related to the opening and closure of the ocean, respectively.
The Paleozoic Jinshajiang ophiolitic melange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys. Basic-intermediate rocks are widespread features in the melange; their formation age is well known, but the petrogenesis has not been well studied, which means that the evolutionary history of the Jinshajiang Ocean is not well constrained. To understand the nature of the melange and the ocean, we present a set of elemental and isotopic data from two typical crustal sequences in two areas of the Jinshajiang ophiolitic melange, Zhiyong and Baimaxueshan. The basalts in the ca. 343 Ma Zhiyong crustal sequence show mid-ocean-ridge basalt-like geochemical compositions with Nb/La ratios of 0.98-1.15 and εNd(t) values of +6.5 to +7.7, indicating that the basalts formed in the spreading ridge of the ocean. In contrast, the 283 Ma Baimaxueshan crustal sequence consists of gabbros and basaltic-andesitic lavas, which have an arc affinity with Nb/La ratios of 0.54-0.67 and εNd(t) values of +5.1 to +6.5. The geochemical differences were not caused by crustal assimilation but reflect mantle metasomatism by fluids dehydrated from the subducting slab. Therefore, we propose that the Zhiyong and Baimaxueshan crustal sequences formed in seafloor spreading and subduction settings, which were related to the opening and closure of the ocean, respectively.
Author Zhong Hong, Zhong Hong
Hu Wenjun, Hu Wenjun
Bai Zhongjie, Bai Zhongjie
Zhu Weiguang, Zhu Weiguang
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Snippet The Paleozoic Jinshajiang ophiolitic melange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys....
Abstract The Paleozoic Jinshajiang ophiolitic mélange in southwest China marks an important branch ocean (i.e., the Jinshajiang Ocean) of the Paleo-Tethys....
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SubjectTerms Ailao Shan
Ailaoshan Ophiolite
Ailaoshan suture zone
alkaline earth metals
Asia
Baimaxueshan
basalts
Benzilan China
Changning-Menglian Ophiolite
China
crust
diabase
Far East
gabbros
Geochemistry
Geophysics
harzburgite
ICP mass spectra
igneous rocks
isotope ratios
isotopes
Jianshajiang suture zone
Jinshajiang Ocean
Jinshajiang ophiolitic melange
Jinshajiang-Ailaoshan Ocean
lanthanum
lava
lithosphere
major elements
mass spectra
melange
metals
metamorphism
metasomatism
mid-ocean ridge basalts
Nd-144/Nd-143
neodymium
niobium
ophiolite
paleo-oceanography
paleogeography
Paleotethys
peridotites
plate tectonics
plutonic rocks
radioactive isotopes
rare earths
rifting
samarium
Sanjiang
sea-floor spreading
serpentinization
Sibumasu China
Sichuan China
Sm-147/Nd-144
solid Earth (tectonophysics)
southwestern China
spectra
Sr-87/Sr-86
stable isotopes
strontium
subduction
suture zones
trace elements
ultramafics
volcanic rocks
whole rock
X-ray fluorescence spectra
Yunnan China
Zhiyong China
Title Rift- and subduction-related crustal sequences in the Jinshajiang ophiolitic melange, SW China; insights into the eastern Paleo-Tethys
URI https://pubs.geoscienceworld.org/gsa/lithosphere/article/11/6/821/574579/Rift-and-subductionrelated-crustal-sequences-in
Volume 11
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