Add to ORKGIn this paper, the author describes the sedimentology and petrography of West Crocker Formation in Sulaman area, Kota Kinabalu, Sabah. West Crocker Formation is part of the accretionary complex in NW Sabah. The beddings are almost vertical and the sediments are all clastic. The facies in West Crocker Formation could be divided into four main groups; i) massive sandstone, ii) silty sandstone, iii) laminated mudstone, ix) carbonaceous shale. The contact between facies shows two main current trends which are strong turbidity current and weak turbidity current
Soft-sediment deformation structures are present within the deep-marine fan of the West Crocker Form...
The Western and Northern part of Sabah, consisting of sedimentary and igneous rocks of Early Cretace...
The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environm...
The Oligocene-Early Miocene of West Crocker Formation is well exposed in the Northwest Sabah, Borne...
Sand injectites are common in the turbidite sequences of the West Crocker Formation (Eocene-Oligocen...
Borneo was positioned in an exceedingly dynamic tectonic area throughout the Tertiary at the edge of...
This study is aimed to study the stratigraphy in southwest Sabah. The study area consists of Temburo...
The Charu Formation of the Kuantan Group is exposed across the Sungai Lembing area in Pahang. This L...
The study area located at the Klias Peninsula consists of the Temburong Formation, Crocker Formation...
The deep marine Crocker Formation in NW Sabah, Malaysia has been well studied in terms of sedimentol...
The increasing population in Kota Kinabalu is proportional to the demand for water resource. Groundw...
The study area is located in the western coast of Sabah between Telipok and Tuaran. The paper presen...
This study focuses on the sedimentological, depositional environment and reservoir quality belongs ...
A geological study was carried out at Parit Sulong area, Johor which has been identified by the prev...
Sandakan Formation (Late Miocene) is exposed across the Sandakan Peninsula in East Sabah and its est...
Soft-sediment deformation structures are present within the deep-marine fan of the West Crocker Form...
The Western and Northern part of Sabah, consisting of sedimentary and igneous rocks of Early Cretace...
The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environm...
The Oligocene-Early Miocene of West Crocker Formation is well exposed in the Northwest Sabah, Borne...
Sand injectites are common in the turbidite sequences of the West Crocker Formation (Eocene-Oligocen...
Borneo was positioned in an exceedingly dynamic tectonic area throughout the Tertiary at the edge of...
This study is aimed to study the stratigraphy in southwest Sabah. The study area consists of Temburo...
The Charu Formation of the Kuantan Group is exposed across the Sungai Lembing area in Pahang. This L...
The study area located at the Klias Peninsula consists of the Temburong Formation, Crocker Formation...
The deep marine Crocker Formation in NW Sabah, Malaysia has been well studied in terms of sedimentol...
The increasing population in Kota Kinabalu is proportional to the demand for water resource. Groundw...
The study area is located in the western coast of Sabah between Telipok and Tuaran. The paper presen...
This study focuses on the sedimentological, depositional environment and reservoir quality belongs ...
A geological study was carried out at Parit Sulong area, Johor which has been identified by the prev...
Sandakan Formation (Late Miocene) is exposed across the Sandakan Peninsula in East Sabah and its est...
Soft-sediment deformation structures are present within the deep-marine fan of the West Crocker Form...
The Western and Northern part of Sabah, consisting of sedimentary and igneous rocks of Early Cretace...
The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environm...