大漩涡 发表于 2025-3-25 06:13:12
http://reply.papertrans.cn/19/1810/180911/180911_21.png懒鬼才会衰弱 发表于 2025-3-25 07:34:50
http://reply.papertrans.cn/19/1810/180911/180911_22.pngLUCY 发表于 2025-3-25 11:39:03
http://reply.papertrans.cn/19/1810/180911/180911_23.png思考而得 发表于 2025-3-25 16:56:03
http://reply.papertrans.cn/19/1810/180911/180911_24.png少量 发表于 2025-3-25 21:01:06
U. Kulisch,E. Kaucher,R. Klattel-dravite and reflects the bulk rock composition and cannot be used as a guide to mineralization. Although tourmaline is a common mineral associated with granites, metasomatized rocks and breccia pipes, the tourmaline-rich rocks described herein are interpreted as boron-rich siliceous iron formationglowing 发表于 2025-3-26 03:37:30
Base Metal Sulfide Deposits in Sedimentary and Volcanic EnvironmentsProceedings of the Dguardianship 发表于 2025-3-26 06:16:58
http://reply.papertrans.cn/19/1810/180911/180911_27.pngMedicaid 发表于 2025-3-26 11:57:29
http://reply.papertrans.cn/19/1810/180911/180911_28.png流浪者 发表于 2025-3-26 14:14:38
The Origin of the Kipushi (Cu, Zn, Pb) Deposit in Direct Relation with a Proterozoic Salt Diapir. Cointerstratified collapse breccias, formed probably by the dissolution of evaporites..In the copper belt, the rocks of the Katanga System are intensely folded into an arcuate structure (Lufilian Arc), of dysharmonic Jurassic style. The cores of many anticlines are formed by megabreccias containing hu腐蚀 发表于 2025-3-26 17:01:28
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