Gangdese

基本解釋

Neogene porphyries from Gangdese: petrological, geochemical characteristics and geodynamic significances.
岡底斯晚第三紀斑巖的巖石學、地球化學及其地球動力學意義
The Gangdese porphyry copper belt is a new discovered ore belt in the South Tibet, China.
岡底斯斑巖銅礦帶是在藏南新發(fā)現(xiàn)的銅礦帶。
Abstract: The Tinggong porphyry copper deposit (PCD) is an important deposit in Gangdese PCD belt.
中文摘要: 廳宮斑巖銅礦床是西藏岡底斯斑巖銅礦帶上重要的礦床之一。
A new silver-polymetallic mineralization belt in parallel with the Gangdese porphyry copper belt was disco-vered on the northern side of the Gangdese Range.
在岡底斯斑巖銅礦帶的北側(cè),發(fā)育一條與之平行的銀多金屬礦化帶。
The Chongjiang porphyric intrusion occurred in the middle of the Gangdese porphyry copper belt in the Southern Tibet plateau.
沖江銅礦床位于岡底斯銅礦帶的中部。