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Volume 23 Issue 3
Jun.  2012
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The late mesozoic granodiorites from the southwest basin in the South China Sea and its tectonic implication

  • Received Date: 2017-03-16
  • The southwest basin is a key to study the origin and development of the South China Sea (SCS). We do not know much about its boundaries, geological history, and the formation of its sea floor because it has a complex and highly regional structural background, notable sediment activity, and yet few floor rocks. Here a granodiorite sample was collected from the southern margin of the southwest basin of the South China Sea. The results indicated that the Ar-40-Ar-39 ages of biotites in the sample are 110.3 +/- 0.5 Ma, suggesting that they were
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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The late mesozoic granodiorites from the southwest basin in the South China Sea and its tectonic implication

  • 1. [ 1 ] China Univ Geosci, Fac Earth Sci, Wuhan 430074, Peoples R China [ 2 ] Hebei United Univ, Coll Min Engn, Tangshan 063009, Peoples R China [ 3 ] Key Lab Mineral Dev & Secur Technol Hebei Prov, Tangshan 063009, Peoples R China [ 4 ] China Univ Geosci, Sch Ocean Sci, Beijing 100083, Peoples R China [ 5 ] Minist Land & Resources China, Guangzhou Marine Geol Survey, Guangzhou 510075, Guangdong, Peoples R China

Abstract: The southwest basin is a key to study the origin and development of the South China Sea (SCS). We do not know much about its boundaries, geological history, and the formation of its sea floor because it has a complex and highly regional structural background, notable sediment activity, and yet few floor rocks. Here a granodiorite sample was collected from the southern margin of the southwest basin of the South China Sea. The results indicated that the Ar-40-Ar-39 ages of biotites in the sample are 110.3 +/- 0.5 Ma, suggesting that they were

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