大陆增生 meaning in Chinese
continental accretion
tectonic accretion
Examples
- Zhou zuyi , 1989 , pre - mesozoic structure of southeast china and its tectonic constraints on east china sea , in : abstract of papers , international symposium on geological - geophysical mapping of the pacific region , yuzhno - sakhalinsk , 112 - 114
周祖翼, 1989 ,利用古地磁资料探讨亚洲东部大陆增生的若干问题,第四届全国古地磁学术会议论文摘要汇编,杭州 - Since twenty years , with the information accumulation , geologists had already cognizant that the transformation of the asia - australia - pacific ocean area during entire virtually is a process of disorganization of gawana landmass and hyperplasia of asia continent . the most complex and important terra segment in the area is the location which links up the eastern part of tethyan and pacific ocean
近二十年来，随着资料的积累，地质学家已经认识到，亚洲?澳洲?太平洋地区在整个显生宙期间的变化实质上是一个冈瓦纳大陆解体和亚洲大陆增生的过程(黄汲清等， 1987 ；殷鸿福等， 1988 ；钟大赉等， 1993 ) ，其中最为复杂和重要的地段就是特提斯东段与太平洋的衔接处。