Add to ORKGThe Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have a complex basin evolution in the Paleo-Tethys. Based on major stratigraphic. geological, geophysical and tectonic phenomena, the Peninsular Malaysia is divided into Western, Central, and Eastern tectonostratigraphic belts. Within the Western Belt, the Kinta Limestone is a voluminous succession, representing 65% of the Paleozoic in the Kinta Valley. Owing to structural and tectono-thermal complexities; sedimentological and paleontological works in these carbonates have proven to be problematic
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
The Gua Musang Formation can be classified into Middle Permian-Middle Triassic sediment comprising c...
Plate tectonic reconstructions of Southeast Asia is quite complicated as the areas are composed of s...
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have...
The limestone hills of the Kinta Valley are remnants of extensive limestone beds, which are part of ...
The Paleozoic limestone of Kinta Valley formed a narrow deformed strip between the Late Triassic - E...
The Kinta Limestone is an important Silurian to Permian age unit in the Western Belt of Peninsular M...
Gunung Kanthan limestone in Chemor, northern part of Kinta Valley, is part the massive Paleozoic Kin...
International audiencePetroleum basins of Western Malaysia are poorly known and their formation is c...
The overall stratigraphy of the Upper Palaeozoic of western Peninsular Malaysia remains unclear. Des...
The Malay Peninsula is characterised by three north-south belts, the Western, Central, and Eastern b...
The Jurassic-Cretaceous (JK) strata in Peninsular Malaysia occur as folded sequences (Tembeling Grou...
Besides tin, the Kinta Valley is known for its lithology and biostratigraphy. Study on some Permian ...
In the eastern side of the Malay Peninsula, thick successions of limestone formations preserve impor...
In Northeast Pahang and South Terengganu, the Kuantan Group and Taweh beds rocks are redefined in te...
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
The Gua Musang Formation can be classified into Middle Permian-Middle Triassic sediment comprising c...
Plate tectonic reconstructions of Southeast Asia is quite complicated as the areas are composed of s...
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have...
The limestone hills of the Kinta Valley are remnants of extensive limestone beds, which are part of ...
The Paleozoic limestone of Kinta Valley formed a narrow deformed strip between the Late Triassic - E...
The Kinta Limestone is an important Silurian to Permian age unit in the Western Belt of Peninsular M...
Gunung Kanthan limestone in Chemor, northern part of Kinta Valley, is part the massive Paleozoic Kin...
International audiencePetroleum basins of Western Malaysia are poorly known and their formation is c...
The overall stratigraphy of the Upper Palaeozoic of western Peninsular Malaysia remains unclear. Des...
The Malay Peninsula is characterised by three north-south belts, the Western, Central, and Eastern b...
The Jurassic-Cretaceous (JK) strata in Peninsular Malaysia occur as folded sequences (Tembeling Grou...
Besides tin, the Kinta Valley is known for its lithology and biostratigraphy. Study on some Permian ...
In the eastern side of the Malay Peninsula, thick successions of limestone formations preserve impor...
In Northeast Pahang and South Terengganu, the Kuantan Group and Taweh beds rocks are redefined in te...
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
The Gua Musang Formation can be classified into Middle Permian-Middle Triassic sediment comprising c...
Plate tectonic reconstructions of Southeast Asia is quite complicated as the areas are composed of s...