怒江断裂带南段道街盆地第四纪构造活动特征

Abstract

Abstract: Since the late Pliocene, a large area of western Yunnan has experienced tectonic movements of tilting uplift, accompanied by different lifting movement among the blocks. In this tectonic context, a series of faulted basins formed in the southern section of the Nujiang fault zone, and Daojie basin is the largest one. The study of Quaternary strata and basin-controlled faults of the Daojie basin in terms of geologic expedition, drilling, surveying profile with virtue deferential GPS indicate that the latest activity of basin-controlled faults of the Daojie basin is the period between middle Pleistocene and late Pleistocene, and the faults within the basin have been active since late Pleistocene.

Key words: Faulted basin, Filled sequence, Structural framework

CLC Number:

P315

CHENG Li, CHEN Guo-xing, SU Gang, LI Guang-tao. Characteristics of the Quaternary Tectonic Activity of the Daojie Basin in the South Section of Nujiang Fault Zone[J]. EARTHQUAKE, 2011, 31(2): 97-105.

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Characteristics of the Quaternary Tectonic Activity of the Daojie Basin in the South Section of Nujiang Fault Zone

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