The Carboniferous and Permian systems are important components of the basement rocks in Thailand and crop out widely. The exceptions are the Khorat Plateau, where they occur in the subsurface but are concealed beneath a thick Mesozoic cover, and in the Chao Phraya Central Plain where they are largely covered by Quaternary sediments but crop out in scattered monadnocks (Fig 5.1). Most Carboniferous and Permian rocks are of shallow-marine facies although siliceous sediments of ancient ocean-bottom origin are also known in places. Continental deposits are quite rare. The Carboniferous System is dominated by siliciclastic rocks except in northernmost Thailand around the Chiang Mai-Mae Hong Son area where there are large carbonate bodies. In contrast, carbonates are the dominant lithology in the Permian System, forming characteristic karst topography in the tropical humid climate. It has been quarried in some areas, such as Saraburi and Ratchaburi, for flagstones and cement production.
In the 1970s and 1980s the Department of Mineral Resources (DMR), Thailand, published a series of 1:250 000 scale geological maps covering the whole of Thailand. That stratigraphic information laid the groundwork for a number of papers on the Carboniferous and Permian systems of this country (Bunopas 1981, 1983, 1992, 1994; DMR 2001, 2007; Raksaskulwong 2002; Assavapatchara et al. 2006). In parallel with those stratigraphical works, more palaeontological aspects of Carboniferous and Permian strata were summarized (Toriyama etal. 1975; Ingavat
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The Geology of Thailand
This is the first volume in the English language to cover the entire range of the geology of Thailand since the joint Thai—US account by Brown et al. exactly 60 years ago. Over this period there has been a phenomenal growth in interest in this core area of SE Asia. This has been led by geologists in Thailand, but with important and highly significant input from geologists based elsewhere in Asia and in Europe, Australasia and North America. Some of that research was prompted by commercial considerations, since Thailand has important energy and mineral resources, while other research has sought to understand better the stratigraphic and structural history, including the plate-tectonic story which Thailand's rocks reveal. This new volume seeks to bring together all of this knowledge into a single accessible book; it is the work of an international team drawn from Thailand, Japan, Australia, USA, Canada, Germany and the UK.