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Figure 1. Coalfields in South Korea<br />
The late Carboniferous to early Triassic Pyeongan Supergroup crops out in the Ogcheon belt<br />
(Figure 1). In the Samcheog Coal Field (SCCF), the largest in South Korea, containing fortyfour<br />
percent of national reserves, the Pyeongan Supergroup was divided by Cheong (1969)<br />
into seven formations; the Manhang, Geumcheon, Jangseong, Hambaegsan, Dosagog, Gohan<br />
and Donggo Formations in ascending order (Figure 2). These mainly consist of sandstone,<br />
shale, coal and some limestone (Figure 3). The detailed lithostratigraphy and depositional<br />
environments of the supergroup have been discussed by Lee & Chough (2006). Up to seven<br />
coal seams are interbedded in the Jangseong and Geumcheon formations. The thickness of<br />
these coal seams varies from 0.6 to 4.0 meters in non-tectonised areas, but local deformation<br />
including folding and thrusting has given rise to local variations of thickness and lateral<br />
continuity. The dips of the coal seam are normally steep, ranging from thirty to eighty degrees.<br />
Surface occurrence of coal seams extends to a maximum of almost 100km in the SCCF. The<br />
rank of coal is classed as anthracite to meta-anthracite.<br />
The late Triassic to early Jurassic Daedong Group, unconformably overlying either<br />
Precambrian gneiss or the Pyeongan Supergroup, occurs in the Ogcheon belt and the<br />
Gyeonggi massif (Figure 1). The so-called Bansong, Nampo and Kimpo Groups are broadly<br />
correlated with the Daedong Group, depending upon the localities of occurrence; however the<br />
precise stratigraphic correlation of the each group is not yet determined. The Daedong Group<br />
mainly consists of conglomerate, sandstone, shale and several horizon of coal. The total<br />
thickness of the sedimentary sequences varies from 400 meters in the case of the Bansong<br />
Group., 1,600 meters for the Kimpo Group and up to 3,000 meters for the Nampo Group<br />
(Reedman and Um 1975). The latter Group includes twenty-five to thirty coal seams in the<br />
Chungnam Coalfield (CNCF, Figure 4)) and id divided into five formations; the Hajo,<br />
New Energy Resources in the <strong>CCOP</strong> Region - Gas Hydrates and Coalbed Methane 121