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- 6198.pdf accessdate "2010-11-27".
- 6198.pdf archivedate "--07-08".
- 6198.pdf author2 "Paul Vella".
- 6198.pdf date "--11-17".
- 6198.pdf date "--11-24".
- 6198.pdf first "Sangad".
- 6198.pdf first1 "Sangad".
- 6198.pdf first2 "Paul".
- 6198.pdf format "PDF 1.8 MB".
- 6198.pdf isCitedBy History_of_Isan.
- 6198.pdf isCitedBy Khorat_Plateau.
- 6198.pdf isCitedBy Zomia_(geography).
- 6198.pdf last "Bunopas".
- 6198.pdf last1 "Bunopas".
- 6198.pdf last2 "Vella".
- 6198.pdf location "Bangkok".
- 6198.pdf page "224".
- 6198.pdf pages "209–229".
- 6198.pdf publisher "Department of Mineral Resources, Bangkok".
- 6198.pdf publisher "National Conference on Geologic Resources of Thailand".
- 6198.pdf quote "...latest Pleistocene early to the Recent regional uplifting must have occurred.".
- 6198.pdf quote "Thailand consists of Shan–Thai and Indochina Microcontinents or Terranes welded together by the subsequently deformed Nan Suture.... During the Middle Triassic Shan–Thai sutured nearly simultaneously to Indochina and to South China, the continent–continent collision being a part of the Indosinian Orogeny and Indochina tended to underthrust Shan–Thai.".
- 6198.pdf title "Geotectonics and Geologic Evolution of Thailand".
- 6198.pdf url 6198.pdf.
- 6198.pdf work "National Conference on "Geologic Resources of Thailand: Potential for Future Development"".