The Origin of the Black Shale Series and Bentonites from the Wufeng Formation in the Southwestern Upper Yangtze: Implications for the Convergence of the Yangtze and Cathaysia Blocks in the Late Ordovician
【摘要】:
Early Paleozoic black organic sediments and bentonites occur widely in the craton basin within the Yangtze block and are gene...

手機(jī)打開
論文排版
