Ordovician paleomagnetism of eastern Yunnan, China
نویسندگان
چکیده
Three magnetic components have been isolated in Ordovician formations of the Yangtze Paraplatform (South China Block). Two of these (Daqing A and Hongshiya B components) yield paleopoles that conform to the Carboniferous to Triassic segment of the apparent polar w•der path for South China, and are therefore interpreted as remagnetizations. The third component (declination/inclination = 30!ø/+66 ø, N = 5 sites, k = 21.4, ct95 = 17 ø) passes the fold test and is interpreted as primary (late Early Ordovician). The palcopole, at 39øS, 236øE, and the paleolatitude of 48øS support an Ordovician position of South China adjacent o
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