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| PubMed | |
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Article by Lu, X. B. |
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Article by Dong, H. C. |
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Article by Jia, H. M. |
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Article by Yuan, Q. |
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Article by Zhu, S. H. |
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Article by Peng, Y. J. |
���ݼ���ʡ������������ص��ݻ�����ʯ�ز������������Բ����ϽӴ���ϵ��ȷ�ϣ���������ɽ�ҵ�ͬλ�����ѧ���ϣ�����ȷ��ϲɽ�������ؾ��������ն���/·���ڡ������DZ���/������ڡ�������/����̹�ڡ�����������/�ж������ڡ�ī������/�˶��ں�Ƥ���ٲ���/����˹�ڵ� 6 �������˶�Ļ����������¹����˶���չ�ڡ����������DZ���/�������ĻΪ������Ļ�������������й����������¸ı��˱���̫ƽ���½��Ե�Ĺ�����ʽ��
Based on the evolution of Cenozoic sedimentary basins and the confirmation of the regional uncon- formity contact relationship in lithostratigraphic sequences in Jilin Province��the authors confirm that the Himalayan (Xishan) structural cycle has experienced six movement episodes including Ypresian/Lutetian��Priabonian/��upe- lian��Chattian/Aquitanian��Serravallian/Tortonian��Messinian/Zanclean and Piacenzian/Gelasian��subsequently�� the Himalayan period gets into the developmental ore of neoteetonics�� The Priabonian/��upelian is the main episode of structural cycle�� which effects the whole eastern China�� even change the structural style of the continental margin of West Pacific Ocean region��