我国中新生代古气候演化及其对盆地砂岩型铀矿的控制作用OACSCDCSTPCD
Paleo-climate evolution in China and its control on the metallization of sandstone type uranium deposit of Meso-Cenozoic basins
文章在分析我国中新生代古气候演化的基础上,指出早侏罗世、中侏罗世及早白垩世、晚白垩世是我国盆地砂岩型铀矿形成的有利古气候期,并在盆地中形成了相应的赋矿层位；建立了我国中新生代产铀盆地3种古气候演化系列；探讨了近代气候对盆地铀成矿的控制作用.
This paper analyzed the climate evolution of China in Meso-cenozoic and indicated that climate in Early Jurassic, Middle Jurassic , Early Cretaceous and Late Cretaceous was favorite for the forming of uranium deposit and produced corresponding uranium bearing strata. The paper have set up the system of paleo-climate evolution in China and discussed the control role of modern climate on uranium metallization in the basins.
陈戴生;刘武生;贾立城
核工业北京地质研究院,北京100029核工业北京地质研究院,北京100029核工业北京地质研究院,北京100029
天文与地球科学
中新生代盆地古气候演化砂岩型铀矿
Meso-Cenozoic basin paleo-climate evolution sandstone type uranium deposit
《铀矿地质》 2011 (6)
321-326,344,7
评论