Karang Paningal gold-ore deposits belong to the epithermal deposits. As hydrothermal deposits, the alter- ation that occurs in this area comprises argillitization, sericitization and silicification. The gold is included within several veins that perform three texture types, namely chalcedony, comb and vuggy. Based on its mineral contents and vein deposit types, mineralization at Karang Paningal took place in two stages that was early epithermal process producing comb-vuggy vein deposit and final epithermal deposit retaining chalcedony vein deposit. Zone of prospective mineralization takes place within vein and rocks beneath and above vein
Phenomena of hydrothermal activity are frequently observed in the studied area (Tirtomoyo), which is...
The research location is located in Paningkaban area and its surrounding areas that included in the ...
The study area (Penjom Gold Deposit, Pahang, Malaysia) lies 30 km east of the major terrane boundary...
Low suphidation (LS) epithermal gold deposits were recently found in the Paningkaban area, Central J...
Senepo area is one of several epithermal mineralization prospects in Southern Mountains of Java Isla...
The southern mountains of western Java have been known to have large gold deposit potential. The Mek...
The report of high potential for epithermal gold deposit indicated vein float assaying gold content ...
The research area is located in Cihonje and Paningkaban Village, Banyumas Regency, Central Java Prov...
Gold mineralization in Kelantan is mainly distributed in the central part of the state, bounded by S...
Gold-mineralized quartz veins at the Trenggalek district of the Southern Mountains Range in East Jav...
The Pongkor gold-silver deposit, formed at Pliocene age (2.05 ± 0.05 Ma) is the largest low-sulfida...
The Kencana Au-Ag low-sulfidation epithermal deposit, situated in the Neogene magmatic arc of Halmah...
The study area is situated in Buladu area, Sumalata district, Gorontalo province, Indonesia. Goronta...
On the basis of the previous studies and reconnaissance survey in the studyarea covering Sangon, Kal...
The Ngerjo area is the location of study area, situated in Pacitan Regency, East Java, Indonesia. Th...
Phenomena of hydrothermal activity are frequently observed in the studied area (Tirtomoyo), which is...
The research location is located in Paningkaban area and its surrounding areas that included in the ...
The study area (Penjom Gold Deposit, Pahang, Malaysia) lies 30 km east of the major terrane boundary...
Low suphidation (LS) epithermal gold deposits were recently found in the Paningkaban area, Central J...
Senepo area is one of several epithermal mineralization prospects in Southern Mountains of Java Isla...
The southern mountains of western Java have been known to have large gold deposit potential. The Mek...
The report of high potential for epithermal gold deposit indicated vein float assaying gold content ...
The research area is located in Cihonje and Paningkaban Village, Banyumas Regency, Central Java Prov...
Gold mineralization in Kelantan is mainly distributed in the central part of the state, bounded by S...
Gold-mineralized quartz veins at the Trenggalek district of the Southern Mountains Range in East Jav...
The Pongkor gold-silver deposit, formed at Pliocene age (2.05 ± 0.05 Ma) is the largest low-sulfida...
The Kencana Au-Ag low-sulfidation epithermal deposit, situated in the Neogene magmatic arc of Halmah...
The study area is situated in Buladu area, Sumalata district, Gorontalo province, Indonesia. Goronta...
On the basis of the previous studies and reconnaissance survey in the studyarea covering Sangon, Kal...
The Ngerjo area is the location of study area, situated in Pacitan Regency, East Java, Indonesia. Th...
Phenomena of hydrothermal activity are frequently observed in the studied area (Tirtomoyo), which is...
The research location is located in Paningkaban area and its surrounding areas that included in the ...
The study area (Penjom Gold Deposit, Pahang, Malaysia) lies 30 km east of the major terrane boundary...