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• W2063750930 abstract "The Upper Carboniferous basaltic Woniusi Formation was sampled at 21 sites from two limbs of a syncline near Baoshan city (25.2°N, 99.3°E), and from a monocline near Yongde county (23.9°N, 99.2°E) for paleomagnetic study. The study area is generally thought to be part of the Shan-Thai-Malay microplate. Thermal demagnetization reveals a single-polarity characteristic remanent magnetization (ChRM) which is carried by both magnetite and hematite, with the former being the dominant mineral in basalt and the latter being the principal carrier in associated tuffaceous basalt and sandstone. The tilt-corrected formation mean from Baoshan (D = 209.2°, I=61.0, α95 =6.7°) confirms the results reported by previous workers, and a positive fold test constrains the ChRM acquisition to be prefolding. The paleomagnetic inclinations determined from this study are similar to that derived from the Devonian rocks from the same area by other workers, indicating a paleolatitude of about 42° for the Baoshan area during the Devono-Carboniferous time. The paleomagnetic declinations, however, present a large difference between the two sampling localities for the Upper Carboniferous as well as between the sampling sites for the Devonian and for the Upper Carboniferous. The paleo-declination difference can be partly explained by the apparent polar wander of Gondwana if the Shan-Thai-Malay microplate was rigidly attached to Gondwanaland during this time interval; the large part of it has to be ascribed to tectonic rotations between the sampling sites. This fact suggests that extreme caution should be exerted when trying to establish an apparent polar wander path for, and to reconstruct the paleo-geographic position of, the Shan-Thai-Malay microplate." @default.
• W2063750930 created "2016-06-24" @default.
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• W2063750930 date "1991-06-01" @default.
• W2063750930 modified "2023-10-17" @default.
• W2063750930 title "Paleomagnetic results from the Upper Carboniferous of the Shan-Thai-Malay block of western Yunnan, China" @default.
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• W2063750930 doi "https://doi.org/10.1016/0040-1951(91)90107-4" @default.
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