Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China
Abstract The world-class Shizhuyuan W–Sn–Mo–Bi deposit is spatially related to the Qianlishan granite complex (QGC) in Hunan Province, China. However, the age and classification of the QGC are still debated, and a better understanding of the temporal genetic relationship between the QGC and the Shiz...
Guardado en:
| Autores principales: | , , , , , , |
|---|---|
| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2021
|
| Materias: | |
| Acceso en línea: | https://doaj.org/article/303211726cbe4473993c0104f344ac34 |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| id |
oai:doaj.org-article:303211726cbe4473993c0104f344ac34 |
|---|---|
| record_format |
dspace |
| spelling |
oai:doaj.org-article:303211726cbe4473993c0104f344ac342021-12-02T11:36:36ZEvidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China10.1038/s41598-021-84902-62045-2322https://doaj.org/article/303211726cbe4473993c0104f344ac342021-03-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-84902-6https://doaj.org/toc/2045-2322Abstract The world-class Shizhuyuan W–Sn–Mo–Bi deposit is spatially related to the Qianlishan granite complex (QGC) in Hunan Province, China. However, the age and classification of the QGC are still debated, and a better understanding of the temporal genetic relationship between the QGC and the Shizhuyuan deposit is essential. Here, we present chemical compositions the intrusive phases of the QGC and the results of detailed zircon U–Pb dating and muscovite Ar–Ar dating of a mineralized greisen vein. Our new zircon laser ablation inductively coupled plasma mass spectrometry U–Pb age data constrain the emplacement of the QGC to 155–151.7 Ma. According to petrological, geochemical and geochronological data and the inferred redox conditions, the QGC can be classified into four phases: P1, porphyritic biotite granites; P2, porphyritic biotite granites; P3, equigranular biotite granite; and P4, granite porphyry dikes. All phases, and especially P1-P3, have elevated concentrations of ore-forming metals and heat-producing elements (U, Th, K; volume heat-producing rate of 5.89–14.03 μWm−3), supplying the metal and heat for the metalogic process of the Shizhuyuan deposit. The Ar–Ar muscovite age (154.0 ± 1.6 Ma) of the mineralized greisen vein in the Shizhuyuan deposit is consistent with the emplacement time of the QGC, suggesting their temporal genetic relationship.Yuzhong LiaoBo ZhaoDehui ZhangLeonid V. DanyushevskyTonglin LiMingqian WuFeng LiuNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-23 (2021) |
| institution |
DOAJ |
| collection |
DOAJ |
| language |
EN |
| topic |
Medicine R Science Q |
| spellingShingle |
Medicine R Science Q Yuzhong Liao Bo Zhao Dehui Zhang Leonid V. Danyushevsky Tonglin Li Mingqian Wu Feng Liu Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| description |
Abstract The world-class Shizhuyuan W–Sn–Mo–Bi deposit is spatially related to the Qianlishan granite complex (QGC) in Hunan Province, China. However, the age and classification of the QGC are still debated, and a better understanding of the temporal genetic relationship between the QGC and the Shizhuyuan deposit is essential. Here, we present chemical compositions the intrusive phases of the QGC and the results of detailed zircon U–Pb dating and muscovite Ar–Ar dating of a mineralized greisen vein. Our new zircon laser ablation inductively coupled plasma mass spectrometry U–Pb age data constrain the emplacement of the QGC to 155–151.7 Ma. According to petrological, geochemical and geochronological data and the inferred redox conditions, the QGC can be classified into four phases: P1, porphyritic biotite granites; P2, porphyritic biotite granites; P3, equigranular biotite granite; and P4, granite porphyry dikes. All phases, and especially P1-P3, have elevated concentrations of ore-forming metals and heat-producing elements (U, Th, K; volume heat-producing rate of 5.89–14.03 μWm−3), supplying the metal and heat for the metalogic process of the Shizhuyuan deposit. The Ar–Ar muscovite age (154.0 ± 1.6 Ma) of the mineralized greisen vein in the Shizhuyuan deposit is consistent with the emplacement time of the QGC, suggesting their temporal genetic relationship. |
| format |
article |
| author |
Yuzhong Liao Bo Zhao Dehui Zhang Leonid V. Danyushevsky Tonglin Li Mingqian Wu Feng Liu |
| author_facet |
Yuzhong Liao Bo Zhao Dehui Zhang Leonid V. Danyushevsky Tonglin Li Mingqian Wu Feng Liu |
| author_sort |
Yuzhong Liao |
| title |
Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| title_short |
Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| title_full |
Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| title_fullStr |
Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| title_full_unstemmed |
Evidence for temporal relationship between the late Mesozoic multistage Qianlishan granite complex and the Shizhuyuan W–Sn–Mo–Bi deposit, SE China |
| title_sort |
evidence for temporal relationship between the late mesozoic multistage qianlishan granite complex and the shizhuyuan w–sn–mo–bi deposit, se china |
| publisher |
Nature Portfolio |
| publishDate |
2021 |
| url |
https://doaj.org/article/303211726cbe4473993c0104f344ac34 |
| work_keys_str_mv |
AT yuzhongliao evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT bozhao evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT dehuizhang evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT leonidvdanyushevsky evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT tonglinli evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT mingqianwu evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina AT fengliu evidencefortemporalrelationshipbetweenthelatemesozoicmultistageqianlishangranitecomplexandtheshizhuyuanwsnmobidepositsechina |
| _version_ |
1718395749818957824 |