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The morphostructures of Kinta Valley karst

  • Muhammad R
  • et al.
Bulletin of the Geological Society of Malaysia (2003) 46 319-328
DOI: 10.7186/bgsm46200353
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Abstract

The trend of Kinta Valley karst structure is mainly along the 310°-350° with minor directions of about 030°, 040°, 055°, 070° and 085°. These trends originated from tectonic stresses and are observed to have controlled the fonnation of certain karst features such as dolines, wangs, caves and collapse. Abstrak:

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APA

Muhammad, R. F., & Tjia, H. D. (2003). The morphostructures of Kinta Valley karst. Bulletin of the Geological Society of Malaysia, 46, 319–328. https://doi.org/10.7186/bgsm46200353

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