Negative lineaments in the granitic bedrock areas of NW Peninsular Malaysia

J. K. Raj, Jabatan Geologi, Universiti Malaya, Kuala Lumpur
1983 Bulletin of the Geological Society of Malaysia  
Negative lineaments in the granilic bedrock an:as of NW Peninsular Malaysia are inlerpreled to reprcscntlhe strikes of fraClureS lhat have developed both before. and as a result of. an approximalely 120·-300· dirccled compression during the Upper Jurassic to Early Tertiary. The fractures pre-datin~this period of compression are furthermore. iruerpreted to be primary fraclures that hal'e formed during lhe cooling of granile batholiths. particularly lhose emplaced during lhe Upper Triassic.
doi:10.7186/bgsm16198306 fatcat:m6hziptbbbg3zf6ibcj6xdgcqu