A revision on the Palaeozoic lithostratigraphy of east Johor has been made. The Palaeozoic of east Johor comprises of the Mersing Formation, Murau Formation, Dohol Formation, Linggiu Formation, Sedili Volcanic, Jasin Volcanic and Pengerang Tuff. The pre-Permian Mersing Formation, the oldest known rock unit is entirely made up of metamorphosed sedimentary rock of shallow marine origin. Unconformably overlying this unit is the Murau Formation which developed in a small continental faulted basin. The siliciclastic Dohol Formation containing late Early to early Middle Permian Sumalayang limestone as well as the Late Permian Linggiu Formation are also unconformably overlying the Mersing Formation, as are the volcanic units of Pengerang Tuff, Sed...
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have...
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
sequence of elastics and carbonates, that are conformable with the Carboniferous, and a late Permian...
Conglomeratic rocks in East Johor are found in the separately three formations that are the Murau, T...
East Johor is mainly composed of Palaeozoic rock, which is covered by three formations, which are M...
The overall stratigraphy of the Upper Palaeozoic of western Peninsular Malaysia remains unclear. Des...
Low grade metamorphic rocks including slate, phyllite, metasandstone with subordinate schist and qua...
The geological map of Peninsular Malaysia shows that the oldest rocks formation in the Eastern Belt ...
The marine sedimentary rocks of the Kampar area, estimated to be more than 5,500 ft thick, can be li...
Volcaniclastic rocks in East Johor Basin are found in a relatively great abundance comprising Sedili...
The study area which is located at the northern most part of Peninsular Malaysia neighbouring Thaila...
Pebbly mudstones for some years in the Paleozoic sequences of south Thailand (Phuket Group or Kaeng ...
The Malay Peninsula is characterised by three north-south belts, the Western, Central, and Eastern b...
The Malay Peninsula can be divided into three distinct mineral belts, viz. the Western Tin Belt, the...
The Permian of Timor in the Lesser Sunda Islands has attracted the attention of palaeontologists sin...
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have...
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
sequence of elastics and carbonates, that are conformable with the Carboniferous, and a late Permian...
Conglomeratic rocks in East Johor are found in the separately three formations that are the Murau, T...
East Johor is mainly composed of Palaeozoic rock, which is covered by three formations, which are M...
The overall stratigraphy of the Upper Palaeozoic of western Peninsular Malaysia remains unclear. Des...
Low grade metamorphic rocks including slate, phyllite, metasandstone with subordinate schist and qua...
The geological map of Peninsular Malaysia shows that the oldest rocks formation in the Eastern Belt ...
The marine sedimentary rocks of the Kampar area, estimated to be more than 5,500 ft thick, can be li...
Volcaniclastic rocks in East Johor Basin are found in a relatively great abundance comprising Sedili...
The study area which is located at the northern most part of Peninsular Malaysia neighbouring Thaila...
Pebbly mudstones for some years in the Paleozoic sequences of south Thailand (Phuket Group or Kaeng ...
The Malay Peninsula is characterised by three north-south belts, the Western, Central, and Eastern b...
The Malay Peninsula can be divided into three distinct mineral belts, viz. the Western Tin Belt, the...
The Permian of Timor in the Lesser Sunda Islands has attracted the attention of palaeontologists sin...
The Southeast Asia terranes derived from the Gondwana margms m the Carboniferous-Triassic time have...
The session on the palaeontology and stratigraphy of South East Asia is introduced by discussing the...
sequence of elastics and carbonates, that are conformable with the Carboniferous, and a late Permian...