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Volume 40 Issue 5
Oct.  2021
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Article Navigation >  CARSOLOGICA SINICA  > 2021  >  40(5): 793-804
WU Jiwen,WU Liangjun,LV Yong,et al.Transpressional structure and its control on development of Yinchangping dolomite karst system in Lushui City, Yunnan[J].Carsologica Sinica,2021,40(05):793-804. doi: 10.11932/karst20210506
Citation: WU Jiwen,WU Liangjun,LV Yong,et al.Transpressional structure and its control on development of Yinchangping dolomite karst system in Lushui City, Yunnan[J].Carsologica Sinica,2021,40(05):793-804. doi: 10.11932/karst20210506
shu

Transpressional structure and its control on development of Yinchangping dolomite karst system in Lushui City, Yunnan

doi: 10.11932/karst20210506
  • 1.

    State Key Laboratory of Geological Processes and Mineral Resources， China University of Geosciences，Beijing 100083， China

  • 2.

    Institute of Karst Geology，CAGS/Key Laboratory of Karst Dynamics，MNR&GZAR，Guilin，Guangxi 541004，China

  • 3.

    College of Earth Sciences， Jilin University， Changchun，Jilin 130061，China

  • 4.

    Faculty of Land Resource Engineering， Kunming University of Science and Technology， Kunming，Yunnan 650093， China

Funds:

 42001011

 2020014, 2020015

 DD20190022

  • Received Date: 2021-03-30
  • Publish Date: 2021-10-25
    Abstract
  • In this study， we conducted a detailed geological and geomorphological survey into the Yinchangping karst system in the dolomite strata of the Shazipo Formation of the middle-upper Permian in Lushui City， western Yunnan. The Yinchangping karst system consists of karst cave system and karst depression where develop 15 sinkholes and many karst trenches with different size and shape. The results of the inversion of the structural stress tensor from the striation on the fault plane and the characteristics of the stress field reflected by the conjugate shear joint as well as the regional geological background， show that the study area is mainly controlled by SEE-NWW compression and NNE-SSW tension stress field during the eocene-early Miocene， forming a NW-direction（N330°）left transpressional structural system，the geometry and kinematic characteristics of which conform to the Riddle shear mode. The depression with the function of water catchment， formed by the NW-direction（N330°）left transpressional structural fault is conductive to the formation depressions by karstification. The intersection of conjugate joints developing in the dissolution depression is a good water-conducting structure which is superimposed in the strike-slip micro-stretching zone to promote dolomite dissolution to form sinkholes. The underground rock strata compressed by tectonic compression slip between the layers form the micro-cracks which are expanded by dissolution to form karst caves developing along inclined rock strata. The river and ridge are systematically left-lateral offset by the left-lateral strike-slip fault， developing the fault cliff and followed by scree accumulation at the foot of the mountain. Under the effects of structural uplift and denudation， the rock walls continue to retreat， and the early karst caves have transformed into dry caves from the frequent attacks of underground rivers. The modern underground river turns into an open current at the downstream of the slope through the underground river outlet.

     

    • WU Jiwen,WU Liangjun,LV Yong,et al.Transpressional structure and its control on development of Yinchangping dolomite karst system in Lushui City, Yunnan[J].Carsologica Sinica,2021,40(05):793-804.
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