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Geological Evolution of Longhushan World Geopark in Relation to Global Tectonics

叶明和 王军鹏 王璐

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Geological Evolution of Longhushan World Geopark in Relation to Global Tectonics

Geological Evolution of Longhushan World Geopark in Relation to Global Tectonics

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出版历程
  • 收稿日期:  2018-07-15
  • 录用日期:  2018-07-15
  • 刊出日期:  2018-07-15

Geological Evolution of Longhushan World Geopark in Relation to Global Tectonics

  • 1. Three Gorges Research Center for Geo-hazards, Ministry of Education, China University of Geosciences, Wuhan 430074, China
  • 2. Longhushan Administrative Committee, Plan-ning Bureau of Yingtan City, Yingtan 335000, China
  • 3. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
  • 4. Three Gorges Research Center for Geo-hazards, Ministry of Education, China University of Geosciences, Wuhan 430074, China
  • 5. College of Marine Geosciences, Ocean University of China, Qingdao

摘要: The South China fold belt has experienced a complex series of tectonic events that span 1.0 billion years of earth history. Longhushan (龙虎山) World Geopark is located on the Proterozoic suture between the Yangtze craton and Cathyasia block and highlights the long history of this belt. Collision of the Cathyasia and Yangtze cratons 1.0 billion years ago was associated with the formation of the Rodinian supercontinent where most of the planet’s landmasses were amalgamated into one block. Jurassic through Early Cretaceous magmatism was associated with the inland migration of the continental margin arc associated with the penetration of a flat slab after subduction of the Kula-Farallon ridge...

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