The Ulu Sokor gold deposit is one of the most famous and largest gold deposits in Malaysia and is located in the Central Gold Belt. This deposit consists of three major orebodies that are related ...
Malaysia is endowed with a number of major sediment-hosted, orogenic gold deposits that lie parallel to but east of the Bentong-Raub Suture Zone, which runs approximately N–S in central Malaysia. The Selinsing gold deposit is one of the major economic deposits in central Malaysia and is hosted by (meta)-sedimentary units.
sets associated with fault-related rocks and hydrothermal alteration zones were identified in the Central gold belt. The results of this study demonstrates the usefulness of PALSAR …
N–S, NNE–SSW, NE–SW and NW–SE, which derived from directional filtering analysis to PALSAR fine and polarimetric data. The pervasive array of N–S faults in the Central Gold Belt and surrounding terrain is mainly linked to the N–S trending of the Suture Zone. N–S striking lineaments are often cut by younger NE–SWand
The Central Gold Belt of Malaysia's gold mineralisation is assumed to be genetically related to the suture [23]. The unit consists of cherts interspersed with a few sandstone layers and cut by ...
The Central Gold Belt of Malaysia's gold mineralisation is assumed to be genetically related to the suture . The unit consists of cherts interspersed with a few sandstone layers and cut by quartz veins. ... Chemostratigraphy of Se and Au in sedimentary and hydrothermal pyrite from black shale and chert in Central gold belt, …
A gap exists in the subsurface geophysical information concerning the Peninsular Malaysian Central gold belts (PMCGB), which this study seeks to address by bridging the gap with the application of combined electrical resistivity (ER), IP, and 3D GIS methods.
Malaysia is highly endowed with potential areas for mineral resources, which has long historical record in gold exploration at various places within the country's peninsula, specifically at the Central Belt of the Peninsular Malaysia (Ariffin & Hewson 2007; Arifin et al. 2019; Chu & Santokh Singh 1986; Li et al. 2015; Yao, Pradhan & Idrees 2017).
The Central "Gold" Belt represents 20 km wide N-S trend in gold mining localities, illustrating the substantial role of hydrothermal fluids in gold development in Malaysia's peninsular particularly in the North Pahang and Kelantan areas [1,2,3,4].
Structural mapping in Peninsular Malaysia is very important for prospecting sediment-hosted/orogenic gold deposits and polymetallic vein-type mineralization along …
The BRSZ is also genetically related to the sediment-hosted/orogenic gold deposits associated with the major lineaments and form-lines in the central gold belt Central Gold Belt of Peninsular ...
the Peninsular Malaysia are located in the Central Gold Belt (CGB) (Ariffin, 2012; Ariffin and Hewson, 2007; Scrivenor, 1931; Yeap, 1993 ). Gold mineralization in this belt is structurally controlled.
A geophysical survey has been carried out to assess the distribution of gold minerals at the Felda Chiku 3, Gua Musang district, Kelantan, Peninsular Malaysia.
The Bentong‐Raub Suture Zone (BRSZ) of Peninsular Malaysia is one of the major structural zones in Sundaland, Southeast Asia. It forms the boundary between the Gondwana‐derived Sibumasu terrane in the west and Sukhothai Arc in the east. The BRSZ is genetically related to the sediment‐hosted/orogenic gold deposits associated with the …
Penjom deposit is an orogenic gold deposit located in the Central Belt of Peninsular Malaysia. Gold mineralization is associated with various styles and textures of quartz‐carbonate veins hosted ...
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As a renowned orogenic lode gold deposit, the Selinsing gold deposit is located in the Central Belt of Peninsular Malaysia. Geologically, the gold deposit is characterized by auriferous quartz veins and fine-grained gold minerals coexisted with sulfides, and the ore body is hosted by low-grade metamorphic sedimentary rocks and …
Semantic Scholar extracted view of "Structural analysis and vein episode of the Penjom Gold Deposit, Malaysia: Implications for gold mineralisation and tectonic history in the Central Belt of Malaysia" by Zakaria Endut et al.
The Central Gold Belt (CGB) of peninsular Malaysia with widespread small-scale gold mining areas and tropical climate has been investigated to explore new potential areas.
Ore-forming fluids in the auriferous district of the Central gold belt in Peninsular Malaysia were studied for their temperature, salinity, and relationship to the surrounding geology.
The Central Gold Belt (CGB) of Malaysia is a major host to gold deposits. Penjom, Raub, Selising and Buffalo reef are major gold mines in CGB. The study area, …
The Penjom gold deposit lies on the eastern side of the Raub‐Bentong Suture line within the Central Belt of Permo‐Triassic rocks, near Kuala Lipis, Pahang, Malaysia.
Separating the two tin belts is the Central Gold Belt, which has gold, base metal, manganese, iron and barite mineralization. This belt extends from the Thailand …
Structural mapping in Peninsular Malaysia is very important for prospecting sediment-hosted/orogenic gold deposits and polymetallic vein-type mineralization along the major lineaments in the Central Gold Belt, Western Tin Belt and Eastern Tin Belt of Peninsular Malaysia.
The BRSZ is genetically related to the sediment-hosted/orogenic gold deposits in the Central Gold Belt of Peninsular Malaysia (Makoundi et al. 2014). Gold is found mainly in the Central Belt of Peninsular Malaysia (Yeap 1993, 2000; Ariffin and Hewson 2007; Ariffin 2012).
Corpus ID: 126532330; Geology, geochemistry and metallogenesis of selected sediment-hosted gold deposits in the central gold belt, Peninsular Malaysia
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To facilitate tracing the structural patterns and investigate the relationship between structural setting and gold mineralization in the Central Gold Belt (CGB) of the …
The Pulai gold deposit is one of the most promising gold prospects in the Central Belt of Peninsular Malaysia. It is found within the Permian-Triassic Gua Musang sequence of metasediments and metavolcanics and in a structurally controlled NE-SW major fault. Various ore minerals, including pyrite, arsenopyrite, chalcopyrite, sphalerite, …