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六盘山地区晚白垩世-新生代初期古构造运动

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现今中国西部印度-欧亚板块碰撞影响的地区在碰撞之前的构造地貌格局是地学界很关注的问题,对先期古构造地貌格局的了解有助于将先期构造事件从后期印度-欧亚板块碰撞事件中剥离出来.本文选现今青藏高原东北缘的六盘山东麓出露的寺口子剖面新生界底部沉积物,通过详尽的沉积学及古水流方向研究,认为六盘山在晚白垩世-新生代初期存在古构造地貌高地,这为Kohistan-Dras岛弧及冈瓦纳大陆的碎片向欧亚大陆聚合在六盘山地区的反映.
Paleo-tectonogeomorphology during Late Cretaceous to Early Cenozoic in Liupanshan Area
The tectonogeomorphology of the area pre-dating the Indian-Eurasian collision in west China draws dramatic attentions of geologists, the understanding of former tectonogeomorphology will help us to rule out the previous tectonic events from the collision. We select the sediments at the bottom of Cenozoic sequences in Sikouzi section, which were re-vealed in the east of Liupanshan situated in the northeast of the Tibetan Plateau, to reveal the pre-dating tectonogeomor-phology of Liupan Shan. Based on detailed sedimentologic and paleocurrent studies, we suggest that a geomorphologic relief existed in Liupanshan during late Cretaceous to early Cenozoic,which possibly resulted from the far-field effects of the assembly of Kohistan-Dras Arc and Gondwana fragments to Eurasian continent.

Liupanshan,late Cretaceous-early Cenozoic,structural landform,the Tibetan plateau

黄建军、吴建勇、吴竹明、朱鲁生、林秀斌

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浙江省地质矿产研究所,杭州 310007

浙江大学地球科学系,杭州 310027

六盘山 晚白垩世-新生代初期 构造地貌 青藏高原

2012

科技通报
浙江省科学技术协会

科技通报

CSTPCDCHSSCD北大核心
影响因子:0.457
ISSN:1001-7119
年,卷(期):2012.28(1)
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