空气
发表于 2025-3-23 10:36:08
https://doi.org/10.1007/978-981-16-7562-1Barite-fluorite deposits; Source of ore-forming material and fluid; Mineralization regularity; Isotope
APO
发表于 2025-3-23 17:53:49
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歌剧等
发表于 2025-3-23 18:13:43
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撕裂皮肉
发表于 2025-3-23 23:32:05
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变量
发表于 2025-3-24 03:41:49
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Resign
发表于 2025-3-24 09:23:54
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方便
发表于 2025-3-24 11:51:28
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multiply
发表于 2025-3-24 15:48:44
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CLAY
发表于 2025-3-24 21:07:39
Zheng Wu,Christoph M. Schimmeleks include the shallow metamorphic clastic rocks of the Banxi Group, the Moraine conglomerate and conglomerate sandstone of the Ediacaran, and the Cambrian sandstone. The shale is mainly Cambrian black shale. Carbonate rocks include Cambrian-Ordovician limestone, bioclastic limestone, dolomitic lime
暖昧关系
发表于 2025-3-25 00:14:31
https://doi.org/10.1007/978-1-4020-6752-5in southeast Sichuan are strictly controlled by the NE-trending fold fault zone. This fault zone is large in scale and the faults cut deep. Although it does not directly host minerals, the ore-forming wall rock alteration and barite-fluorite mineralization developed along the belt, and the NW-trendi