THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM)
Based on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song‐Chai gneiss‐granite massif (Northern Vietnam), the long‐term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of th...
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2019-06-01
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| Series: | Геодинамика и тектонофизика |
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| Online Access: | https://www.gt-crust.ru/jour/article/view/845 |
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| author | A. G. Vladimirov A. V. Travin Phan Luu Anh N. G. Murzintsev I. Yu. Annikova E. I. Mikheev Nguyen Anh Duong Tran Thi Man Tran Thi Lan |
| author_facet | A. G. Vladimirov A. V. Travin Phan Luu Anh N. G. Murzintsev I. Yu. Annikova E. I. Mikheev Nguyen Anh Duong Tran Thi Man Tran Thi Lan |
| author_sort | A. G. Vladimirov |
| collection | DOAJ |
| description | Based on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song‐Chai gneiss‐granite massif (Northern Vietnam), the long‐term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of the granitoid batholith and mathematical modeling of its thermal history shows that the magmatic chamber should be considered as a thermal trap at the lower level of the crust, which preserved residual granite melts for a long time. Activation of the magmatic chamber occurs in post‐collisional strike‐slip fault zones and is accompanied by tectonic exhumation of large crustal segments. As a result, the batholith is transformed into a Cordilleran‐type metamorphic core complex, residual rare‐metal melts are emplaced, and, commercial deposits are thus formed. |
| format | Article |
| id | doaj-art-7b5119cd7a754d0ab43ff116749f699f |
| institution | Matheson Library |
| issn | 2078-502X |
| language | English |
| publishDate | 2019-06-01 |
| publisher | Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
| record_format | Article |
| series | Геодинамика и тектонофизика |
| spelling | doaj-art-7b5119cd7a754d0ab43ff116749f699f2025-08-04T14:27:22ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2019-06-0110234737310.5800/GT-2019-10-2-0418416THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM)A. G. Vladimirov0A. V. Travin1Phan Luu Anh2N. G. Murzintsev3I. Yu. Annikova4E. I. Mikheev5Nguyen Anh Duong6Tran Thi Man7Tran Thi Lan8V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS; Novosibirsk State University; Tomsk State UniversityV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS; Novosibirsk State University; Tomsk State UniversityInstitute of Geological Sciences, Vietnam Academy of Science and TechnologyV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS; Novosibirsk State University; Tomsk State UniversityV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS; Novosibirsk State UniversityInstitute of Geological Sciences, Vietnam Academy of Science and TechnologyInstitute of Geological Sciences, Vietnam Academy of Science and TechnologyInstitute of Geological Sciences, Vietnam Academy of Science and TechnologyBased on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song‐Chai gneiss‐granite massif (Northern Vietnam), the long‐term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of the granitoid batholith and mathematical modeling of its thermal history shows that the magmatic chamber should be considered as a thermal trap at the lower level of the crust, which preserved residual granite melts for a long time. Activation of the magmatic chamber occurs in post‐collisional strike‐slip fault zones and is accompanied by tectonic exhumation of large crustal segments. As a result, the batholith is transformed into a Cordilleran‐type metamorphic core complex, residual rare‐metal melts are emplaced, and, commercial deposits are thus formed.https://www.gt-crust.ru/jour/article/view/845granitoid batholithmetamorphic core complexgeochronologythermochronologymathematical modelingvietnamsong‐chai massifmetallogenic prediction |
| spellingShingle | A. G. Vladimirov A. V. Travin Phan Luu Anh N. G. Murzintsev I. Yu. Annikova E. I. Mikheev Nguyen Anh Duong Tran Thi Man Tran Thi Lan THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) Геодинамика и тектонофизика granitoid batholith metamorphic core complex geochronology thermochronology mathematical modeling vietnam song‐chai massif metallogenic prediction |
| title | THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) |
| title_full | THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) |
| title_fullStr | THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) |
| title_full_unstemmed | THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) |
| title_short | THERMOCHRONOLOGY OF GRANITOID BATHOLITHS AND THEIR TRANSFORMATION INTO METAMORPHIC CORE COMPLEXES (EXAMPLE OF SONG‐CHAI MASSIF, NORTHERN VIETNAM) |
| title_sort | thermochronology of granitoid batholiths and their transformation into metamorphic core complexes example of song chai massif northern vietnam |
| topic | granitoid batholith metamorphic core complex geochronology thermochronology mathematical modeling vietnam song‐chai massif metallogenic prediction |
| url | https://www.gt-crust.ru/jour/article/view/845 |
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