Control of favorable lithology on Jinlongshan micro-fine disseminated gold deposits, southern Qinling Mountains

2002 ◽  
Vol 45 (2) ◽  
pp. 123-132 ◽  
Author(s):  
Liqing Zhao ◽  
Zhongyan Feng
Keyword(s):  
Gold Deposits ◽  
Qinling Mountains

Selenium Enrichment in Cambrian Stratabound Gold Deposits in the Western Qinling Mountains

2010 ◽  
Vol 71 (4) ◽  
pp. 423-432 ◽  
Author(s):  
Liu Jiajun ◽  
Zheng Minghua ◽  
Liu Jianming ◽  
Zhou Yufeng ◽  
Gu Xuexiang ◽  
...  
Keyword(s):  
Gold Deposits ◽  
Qinling Mountains ◽  
Western Qinling

Gold deposits in the Xiaoqinling-Xiong'ershan region, Qinling Mountains, central China

2002 ◽  
Vol 37 (3-4) ◽  
pp. 306-325 ◽  
Author(s):  
Jingwen Mao ◽  
Richard Goldfarb ◽  
Zhengwei Zhang ◽  
Wenyi Xu ◽  
Yumin Qiu ◽  
...  
Keyword(s):  
Gold Deposits ◽  
Central China ◽  
Qinling Mountains

Au-Se Paragenesis in Cambrian Stratabound Gold Deposits, Western Qinling Mountains, China

2000 ◽  
Vol 42 (11) ◽  
pp. 1037-1045 ◽  
Author(s):  
Liu Jiajun ◽  
Liu Jianming ◽  
Zheng Minghua ◽  
Liu Xianfan
Keyword(s):  
Gold Deposits ◽  
Qinling Mountains ◽  
Western Qinling

Studi Awal Geologi di Daerah Beruang Kanan Kabupaten Gunung Mas Propinsi Kalimantan Tengah

PROMINE ◽  
2018 ◽  
Vol 6 (1) ◽  
pp. 1-11
Author(s):  
Retno Anjarwati ◽  
Arifudin Idrus ◽  
Lucas Donny Setijadji
Keyword(s):  
Gold Mineralization ◽  
Volcanic Rocks ◽  
Gold Deposits ◽  
Central Kalimantan ◽  
Magmatic Arc ◽  
Tertiary Sediment ◽  
Copper Gold ◽  
Regional Tectonic ◽  
Mineralization Processes ◽  
High Yields

The regional tectonic conditions of the KSK Contract of Work are located in the mid-Tertiary magmatic arc (Carlile and Mitchell, 1994) which host a number of epithermal gold deposits (eg, Kelian, Indon, Muro) and significant prospects such as Muyup, Masupa Ria, Gunung Mas and Mirah. Copper-gold mineralization in the KSK Contract of Work is associated with a number of intrusions that have occupied the shallow-scale crust at the Mesozoic metamorphic intercellular junction to the south and continuously into the Lower Tertiary sediment toward the water. This intrusion is interpreted to be part of the Oligocene arc of Central Kalimantan (in Carlile and Mitchell 1994) Volcanic rocks and associated volcanoes are older than intrusions, possibly aged Cretaceous and exposed together with all three contacts (Carlile and Mitchell, 1994) some researchers contribute details about the geological and mineralogical background, and some papers for that are published for the Beruang Kanan region and beyond but no one can confirm the genesis type of the Beruang Kanan region The mineralization of the Beruang Kanan area is generally composed by high yields of epithermal sulphide mineralization. with Cu-Au mineralization This high epithermal sulphide deposition coats the upper part of the Cu-Au porphyry precipitate associated with mineralization processes that are generally controlled by the structure

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