摘要
We report paleomagnetic results from Late Carboniferous-Late Permian strata in eastern Tibet (China), aim to clarify the tectonic and paleogeographic evolution of the northern Qiangtang-Qamdo block, which is a key to the study of plate boundary between the Gondwanaland and Eurasia during the Late Paleozoic time. Two hundred and nineteen samples-including limestone, muddy siltstone, basalt, lava, and tuff were collected at 24 sites in the Upper Carboniferous and Middle-Upper Permian successions, respectively.