Petrogenesis and tectonic environment of the Middle Permian Luerma igneous complex in the southern Lhasa subterrane, Tibet: Evidence from geochemistry; Rb–Sr, Sm–Nd, and Lu–Hf isotopes; and zircon U–Pb geochronology
Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian Luerma igneous complex, which is situated in the western Gangdese magmatic belt of the southern Lhasa subterrane, western Tibet, can be divi...
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| Published in | Geological journal (Chichester, England) Vol. 58; no. 8; pp. 3026 - 3042 |
|---|---|
| Main Authors | , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Hoboken, USA
John Wiley & Sons, Inc
01.08.2023
Wiley Subscription Services, Inc |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian Luerma igneous complex, which is situated in the western Gangdese magmatic belt of the southern Lhasa subterrane, western Tibet, can be divided into four or more rock types, including foid gabbro, amphibole gabbro, monzogabbro, and pyroxene‐bearing monzodiorite. Through zircon U–Pb dating using laser ablation–inductively coupled plasma–mass spectrometry, the age of the Luerma igneous complex is determined to be ~261 Ma. The complex is rich in titanium, iron, magnesium, and total alkalis, with medium to high levels of calcium, potassium and aluminium, as well as low levels of silicon. Therefore, it is classified as a shoshonite–latite rock series. The complex is relatively enriched in light rare earth elements and high‐field‐strength elements, without obvious Eu and Ce anomalies. These rocks exhibit relatively low (87Sr/86Sr)i values, high εNd(t) values, and high εHf(t) values. The geochemical and isotopic characteristics indicate that the magmas are derived from partial melting of the upper mantle in an intraplate tectonic environment. The new data presented here provide supplementary evidence for the initial rifting of the Lhasa terrane from the northern margin of Gondwana during the Middle Permian. These data also confirm that the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean occurred in the Middle Permian.
(a) Simplified tectonic map of the Qinghai–Tibet Plateau, (b) simplified tectonic map of the Lhasa terrane, (c) simplified geological map of the Luerma area. |
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| AbstractList | Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian Luerma igneous complex, which is situated in the western Gangdese magmatic belt of the southern Lhasa subterrane, western Tibet, can be divided into four or more rock types, including foid gabbro, amphibole gabbro, monzogabbro, and pyroxene‐bearing monzodiorite. Through zircon U–Pb dating using laser ablation–inductively coupled plasma–mass spectrometry, the age of the Luerma igneous complex is determined to be ~261 Ma. The complex is rich in titanium, iron, magnesium, and total alkalis, with medium to high levels of calcium, potassium and aluminium, as well as low levels of silicon. Therefore, it is classified as a shoshonite–latite rock series. The complex is relatively enriched in light rare earth elements and high‐field‐strength elements, without obvious Eu and Ce anomalies. These rocks exhibit relatively low (87Sr/86Sr)i values, high εNd(t) values, and high εHf(t) values. The geochemical and isotopic characteristics indicate that the magmas are derived from partial melting of the upper mantle in an intraplate tectonic environment. The new data presented here provide supplementary evidence for the initial rifting of the Lhasa terrane from the northern margin of Gondwana during the Middle Permian. These data also confirm that the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean occurred in the Middle Permian. Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian Luerma igneous complex, which is situated in the western Gangdese magmatic belt of the southern Lhasa subterrane, western Tibet, can be divided into four or more rock types, including foid gabbro, amphibole gabbro, monzogabbro, and pyroxene‐bearing monzodiorite. Through zircon U–Pb dating using laser ablation–inductively coupled plasma–mass spectrometry, the age of the Luerma igneous complex is determined to be ~261 Ma. The complex is rich in titanium, iron, magnesium, and total alkalis, with medium to high levels of calcium, potassium and aluminium, as well as low levels of silicon. Therefore, it is classified as a shoshonite–latite rock series. The complex is relatively enriched in light rare earth elements and high‐field‐strength elements, without obvious Eu and Ce anomalies. These rocks exhibit relatively low ( 87 Sr/ 86 Sr) i values, high ε Nd (t) values, and high ε Hf (t) values. The geochemical and isotopic characteristics indicate that the magmas are derived from partial melting of the upper mantle in an intraplate tectonic environment. The new data presented here provide supplementary evidence for the initial rifting of the Lhasa terrane from the northern margin of Gondwana during the Middle Permian. These data also confirm that the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean occurred in the Middle Permian. Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian Luerma igneous complex, which is situated in the western Gangdese magmatic belt of the southern Lhasa subterrane, western Tibet, can be divided into four or more rock types, including foid gabbro, amphibole gabbro, monzogabbro, and pyroxene‐bearing monzodiorite. Through zircon U–Pb dating using laser ablation–inductively coupled plasma–mass spectrometry, the age of the Luerma igneous complex is determined to be ~261 Ma. The complex is rich in titanium, iron, magnesium, and total alkalis, with medium to high levels of calcium, potassium and aluminium, as well as low levels of silicon. Therefore, it is classified as a shoshonite–latite rock series. The complex is relatively enriched in light rare earth elements and high‐field‐strength elements, without obvious Eu and Ce anomalies. These rocks exhibit relatively low (87Sr/86Sr)i values, high εNd(t) values, and high εHf(t) values. The geochemical and isotopic characteristics indicate that the magmas are derived from partial melting of the upper mantle in an intraplate tectonic environment. The new data presented here provide supplementary evidence for the initial rifting of the Lhasa terrane from the northern margin of Gondwana during the Middle Permian. These data also confirm that the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean occurred in the Middle Permian. (a) Simplified tectonic map of the Qinghai–Tibet Plateau, (b) simplified tectonic map of the Lhasa terrane, (c) simplified geological map of the Luerma area. |
| Author | Cao, Huawen Song, Wenjie Nie, Fei Li, Guangming Huang, Yong Ma, Dongfang Li, Wenchang Huang, Hanxiao Liu, Hong Li, Youguo |
| Author_xml | – sequence: 1 givenname: Hong orcidid: 0000-0002-2167-9396 surname: Liu fullname: Liu, Hong organization: Chengdu University of Technology – sequence: 2 givenname: Guangming surname: Li fullname: Li, Guangming organization: Chengdu Center, China Geological Survey (Geosciences Innovation Center of Southwest China) – sequence: 3 givenname: Wenchang surname: Li fullname: Li, Wenchang email: lwcyndd@163.com organization: Kunming University of Science and Technology – sequence: 4 givenname: Dongfang surname: Ma fullname: Ma, Dongfang email: mdongfang@foxmail.com organization: Chengdu Center, China Geological Survey (Geosciences Innovation Center of Southwest China) – sequence: 5 givenname: Hanxiao surname: Huang fullname: Huang, Hanxiao organization: Chengdu University of Technology – sequence: 6 givenname: Huawen orcidid: 0000-0002-3703-5843 surname: Cao fullname: Cao, Huawen organization: Chengdu Center, China Geological Survey (Geosciences Innovation Center of Southwest China) – sequence: 7 givenname: Youguo surname: Li fullname: Li, Youguo organization: Chengdu University of Technology – sequence: 8 givenname: Yong surname: Huang fullname: Huang, Yong organization: China Geological Survey – sequence: 9 givenname: Fei surname: Nie fullname: Nie, Fei organization: China Geological Survey – sequence: 10 givenname: Wenjie surname: Song fullname: Song, Wenjie organization: Institute of Disaster Prevention |
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| Snippet | Due to the lack of corresponding magmatic records, the timing of the opening of the Yarlung–Tsangpo Neo‐Tethyan Ocean remains controversial. The Middle Permian... |
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| SubjectTerms | Ablation Alkalis Aluminium Aluminum Anomalies Calcium Daggyai Co Earth mantle Gabbro Geochemistry Geochronology Geochronometry Gondwana Inductively coupled plasma mass spectrometry Isotopes Laser ablation Magnesium Mass spectrometry Mass spectroscopy Middle Permian opening of the Neo‐Tethyan Ocean Permian Petrogenesis Potassium Radiometric dating Rare earth elements Rifting Rock Rocks Strontium 87 Strontium isotopes Tectonics Upper mantle within‐plate basalt Yawa Zircon |
| Title | Petrogenesis and tectonic environment of the Middle Permian Luerma igneous complex in the southern Lhasa subterrane, Tibet: Evidence from geochemistry; Rb–Sr, Sm–Nd, and Lu–Hf isotopes; and zircon U–Pb geochronology |
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