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uot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>uot;COLOR: black; mso-font-kerning: 18.0pt" lang=EN-US>uot;Times New Roman">SHRIMP Zircon U-Pb Dating of the Early Jurassic Magmatic Rocks in uot;urn:schemas-microsoft-com:office:smarttags" />uot;on">Dongkeng uot;on">Basin, uot;on">South uot;on">Jiangxi uot;on">Province, and the Later Tectono-Thermal Events in Southern Jiangxi and uot;on">Northern Guangdong Provincesuot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>uot;urn:schemas-microsoft-com:office:office" />

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摘要
ummary name="EnDivSummary">Besides the ages of the Early Jurassic Xialan complex in northern Guangdong Province, this paper reports the SHRIMP zircon U-Pb ages of magmatic rocks in Dongkeng and Linjiang basins, southern Jiangxi areas, southeastern China. The SHRIMP zircon U-Pb ages of 193±2 Ma for granodiorite and 196±1 Ma for gabbro-diabase from Hanhu, Dongkeng Basin, show that the mixed Hanhu complex intruded in the Early Jurassic. Field observation indicates that the gabbro-diabase coexists with syenite in granodiorite, and that the basic components enter the syenite. These rocks, in turn, influenced the Hanhu and Xialan complexs. The confirmation of these tectono-magmatic events will be helpful to understand the Early Jurassic tectonic evolution in this area.

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