Batdabong Fold Complex in Khlong Had Area, Sa Kaeo, Eastern

A weak lava flow structure which characterised by the alignment of prismatic K-fedspar Complex Key geosite to understand the mechanism of the intrusion

In the latter part, Permian-Triassic serpentinite and basalt ap- pear to have formed NE-SW parallel belts Podiform chromite and pillow lava are recognized in

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topone987 They occur on dissected lava flows and erosion surfaces relief is These include Chai Badan, Loei series and Slope Complex ANALYSIS RESULTS