Middle Paleozoic convergent orogenic belts in western Inner Mongolia (China): framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt
Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB), Hunshandake Block (HB), Northern Orogenic Belt (NOB), South Mongoli...
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| Published in | Gondwana research Vol. 23; no. 4; pp. 1342 - 1364 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.05.2013
Elsevier |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB), Hunshandake Block (HB), Northern Orogenic Belt (NOB), South Mongolia microcontinent (SMM), and Southern margin of Ergun Block (SME), suggesting that the tectonic framework of the CAOB in western Inner Mongolia is characterized by an accretion of different blocks and orogenic belts. The SOB includes, from north to south, fold belt, mélange, arc-pluton belt, and retroarc foreland basin, representing a southern subduction–collision system between the NCC and HB blocks during 500–440Ma. The NOB consists also of four units: arc-pluton belt, mélange, foreland molasse basin, and fold belt, from north to south, representing a northern subduction–collision system between the HB and SMM blocks during 500–380Ma. From the early Paleozoic, the Paleo-Asian oceanic domains subducted to the north and the south, resulting in the forming of the SOB and the NOB in 410Ma and 380Ma, respectively. This convergent orogenic system, therefore, constrained the consumption process of the Paleo-Asian Ocean in western Inner Mongolia. A double subduction–collision accretionary process is the dominant geodynamic feature for the eastern part of the CAOB during the early to middle Paleozoic.
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► We describe a Southern and a Northern orogenic belts in western Inner Mongolia. ► They constitute a middle Paleozoic convergent orogenic system. ► A double subduction–collision process led to closure of eastern Paleo-Asian Ocean. |
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| AbstractList | Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB), Hunshandake Block (HB), Northern Orogenic Belt (NOB), South Mongolia microcontinent (SMM), and Southern margin of Ergun Block (SME), suggesting that the tectonic framework of the CAOB in western Inner Mongolia is characterized by an accretion of different blocks and orogenic belts. The SOB includes, from north to south, fold belt, mélange, arc-pluton belt, and retroarc foreland basin, representing a southern subduction–collision system between the NCC and HB blocks during 500–440Ma. The NOB consists also of four units: arc-pluton belt, mélange, foreland molasse basin, and fold belt, from north to south, representing a northern subduction–collision system between the HB and SMM blocks during 500–380Ma. From the early Paleozoic, the Paleo-Asian oceanic domains subducted to the north and the south, resulting in the forming of the SOB and the NOB in 410Ma and 380Ma, respectively. This convergent orogenic system, therefore, constrained the consumption process of the Paleo-Asian Ocean in western Inner Mongolia. A double subduction–collision accretionary process is the dominant geodynamic feature for the eastern part of the CAOB during the early to middle Paleozoic.
[Display omitted]
► We describe a Southern and a Northern orogenic belts in western Inner Mongolia. ► They constitute a middle Paleozoic convergent orogenic system. ► A double subduction–collision process led to closure of eastern Paleo-Asian Ocean. Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB), Hunshandake Block (HB), Northern Orogenic Belt (NOB), South Mongolia microcontinent (SMM), and Southern margin of Ergun Block (SME), suggesting that the tectonic framework of the CAOB in western Inner Mongolia is characterized by an accretion of different blocks and orogenic belts. The SOB includes, from north to south, fold belt, mélange, arc-pluton belt, and retroarc foreland basin, representing a southern subduction-collision system between the NCC and HB blocks during 500-440 Ma. The NOB consists also of four units: arc-pluton belt, mélange, foreland molasse basin, and fold belt, from north to south, representing a northern subduction-collision system between the HB and SMM blocks during 500-380 Ma. From the early Paleozoic, the Paleo-Asian oceanic domains subducted to the north and the south, resulting in the forming of the SOB and the NOB in 410 Ma and 380 Ma, respectively. This convergent orogenic system, therefore, constrained the consumption process of the Paleo-Asian Ocean in western Inner Mongolia. A double subduction-collision accretionary process is the dominant geodynamic feature for the eastern part of the CAOB during the early to middle Paleozoic. |
| Author | Charvet, Jacques Xu, Bei Chen, Yan Shi, Guanzhong Zhao, Pan |
| Author_xml | – sequence: 1 givenname: Bei surname: Xu fullname: Xu, Bei email: bxu@pku.edu.cn organization: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Peking University, Beijing, 100871, China – sequence: 2 givenname: Jacques surname: Charvet fullname: Charvet, Jacques organization: Institut des Sciences de la Terre d'Orléans, UMR 7327 Université d'Orléans-INSU/CNRS, 1A rue de la Férollerie, 45071 Orléans, Cedex 2, France – sequence: 3 givenname: Yan surname: Chen fullname: Chen, Yan organization: Institut des Sciences de la Terre d'Orléans, UMR 7327 Université d'Orléans-INSU/CNRS, 1A rue de la Férollerie, 45071 Orléans, Cedex 2, France – sequence: 4 givenname: Pan surname: Zhao fullname: Zhao, Pan organization: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Peking University, Beijing, 100871, China – sequence: 5 givenname: Guanzhong surname: Shi fullname: Shi, Guanzhong organization: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Peking University, Beijing, 100871, China |
| BackLink | https://insu.hal.science/insu-00707174$$DView record in HAL |
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| Keywords | Central Asian Orogenic Belt Paleo-Asian Ocean Mélange, foreland basin Inner Mongolia mélange foreland basin |
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| Snippet | Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including,... |
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| SubjectTerms | Central Asian Orogenic Belt Earth Sciences Environmental Sciences Global Changes Inner Mongolia Mélange, foreland basin Paleo-Asian Ocean Sciences of the Universe Tectonics |
| Title | Middle Paleozoic convergent orogenic belts in western Inner Mongolia (China): framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt |
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