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IS THERE A PALEOCONTINENTAL NEUCLEUS IN CENTRAL SICHUAN

Luo Zhili  
Some geologists called the Central Sichuan Block a paleocont inentalneucleus. Based on the two deep wells drilled into the basement of thePresinian System in Weiyuan and Longnusi structures and new data obtainedin thin section analysis and chemical analysis of cores, this paper disagreeswith this view point. Instead, considering the geochronological study in theneighbouring Xikang--Yunnan Geoaxis region and data on the formation anddevelopment of the Yangtze Paleoplate, we believe the basement of theCentral Sichuan Block is a "pa1eo--arc Neucleus" in the Xikang--Yunnan-central Sichuan--western Hubei Paleoisland Arc. This idea should be furtherproved and discussed in the study of crustal evolution in South China.
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