Oil shale deposits are known to occur in several areas of Thailand. Perhaps the most important de-posit occurs at Mae Sod, in Tak Province, western Thailand. Other well-known deposits are Li in Lamphun Province, Ko Kha District, Lampang Province, and Krabi in the southern peninsular region. The geological age of all these deposits is late Tertiary, as demonstrated by the presence of the lossils from the oil shale of the Mae Sod series, for example, fish of.the Ostariophysian family Cyprini-dae. In Mae Sod, rich oil shale deposits occupy several small coal-bearing deposits within a larger basin ex-tending westward into the Amherst District of east-ern Burma (Fig. 1). The basin is one of the inter
The southern part of the Central Plain in Thailand is blanketed with a two part sequence here termed...
The first industrial oil in the Timan-Pechora oil and gas province was obtained in 1929. By now more...
The mechanism of formation of lacustrine deposits within stable orogenic belts and their potential f...
Cenozoic deposits occur in many small intermontane basins, especially in northern Thailandin the Cha...
Fang Oilfield is the oldest oilfield in Thailand and is still producing oil. The first oil seepage w...
Recent trends in petroleum production have focused on developing unconventional gas reservoirs such ...
Oil-shale deposits are in many parts of the world. They range in age from Cambrian to Tertiary and w...
World oil reserves in oil shales (1. 2 to 2 trillion barrels) are at least 4 times as large as prove...
The Wang Phar tungsten deposits are located 32 km west-southwest by road from Hatyai, Southern Thail...
Shale oil and gas was widely distributed and has huge potential reserve. The quick development of sh...
Liquid-rich hydrocarbons in shale strata include two kinds of resources, i.e. tight oil and shale oi...
As a consequence of exploration for hydrocarbons, and of research programmes conducted by academic a...
Oil shale, a carbonaceous rock which occurs abundantly in the earth`s crust, has been investigated f...
Oil shale is a crucial unconventional energy source to supplement conventional oil and gas. The oil ...
Abstract: A deep understanding of the basic geologic characteristics of the fine-grained shale layer...
The southern part of the Central Plain in Thailand is blanketed with a two part sequence here termed...
The first industrial oil in the Timan-Pechora oil and gas province was obtained in 1929. By now more...
The mechanism of formation of lacustrine deposits within stable orogenic belts and their potential f...
Cenozoic deposits occur in many small intermontane basins, especially in northern Thailandin the Cha...
Fang Oilfield is the oldest oilfield in Thailand and is still producing oil. The first oil seepage w...
Recent trends in petroleum production have focused on developing unconventional gas reservoirs such ...
Oil-shale deposits are in many parts of the world. They range in age from Cambrian to Tertiary and w...
World oil reserves in oil shales (1. 2 to 2 trillion barrels) are at least 4 times as large as prove...
The Wang Phar tungsten deposits are located 32 km west-southwest by road from Hatyai, Southern Thail...
Shale oil and gas was widely distributed and has huge potential reserve. The quick development of sh...
Liquid-rich hydrocarbons in shale strata include two kinds of resources, i.e. tight oil and shale oi...
As a consequence of exploration for hydrocarbons, and of research programmes conducted by academic a...
Oil shale, a carbonaceous rock which occurs abundantly in the earth`s crust, has been investigated f...
Oil shale is a crucial unconventional energy source to supplement conventional oil and gas. The oil ...
Abstract: A deep understanding of the basic geologic characteristics of the fine-grained shale layer...
The southern part of the Central Plain in Thailand is blanketed with a two part sequence here termed...
The first industrial oil in the Timan-Pechora oil and gas province was obtained in 1929. By now more...
The mechanism of formation of lacustrine deposits within stable orogenic belts and their potential f...