Characteristics of geological, geological structure, a Thai-bend (Folded Belt) and was cut off with a fault (Faulte) is. Complications of granite as the gap at khotkhong and later they were to become, by heat and pressure cause some stone pieces become granite mountains region in the North, West and South, where the majority of age, era o solo phali Ignatius (Palaozoie) -Plateau Northeast is composed of sandstone and schist of the phali era, o solo Ignatius (Palaozoie) around the edge, West and southwest of the Khorat plateau and mountains. The East will have a structured stones bend of video phali era solo Ignatius (Palaozoie) The country's central-Thai is a land basin (Basin) is a large accumulation of sediment layer, light layer of stone age era of the sea no solo Janda (Cenozoic), which consists of the Internet age's leading ocean sediments (Tertiary) and on the floor of these sediments is covered with sedimentary deposit gravel rock of ages quarter binary (Quaternary)
การแปล กรุณารอสักครู่..
![](//thimg.ilovetranslation.com/pic/loading_3.gif?v=b9814dd30c1d7c59_8619)