五行打油诗
发表于 2025-3-25 04:43:48
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混合
发表于 2025-3-25 11:11:45
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Overdose
发表于 2025-3-25 13:55:57
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ARCHE
发表于 2025-3-25 17:10:08
Zeng Yi,Dudley L. Poston,Danan Gution regularity. According to the .Sr/.Sr ratio, trace element and isotopic analysis results, the Cambrian–Ordovician carbonate strata could provide sufficient Ca for mineralization, and the source of Ca was most likely a multi-source. The Lower Cambrian Niutitang Formation (regional) in the study a
incontinence
发表于 2025-3-25 23:00:46
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Allure
发表于 2025-3-26 01:36:51
Element Geochemistry,stance was relatively long. The obtained Eu and Ce anomalies reflect that the ore was formed in an open system with high oxygen fugacity. According to the Tb/Ca-Tb/La and La/Yb-∑REE diagrams, the barite-fluorite deposits in the study area were of hydrothermal origin, magmatic fluids were not involve
jagged
发表于 2025-3-26 07:29:01
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适宜
发表于 2025-3-26 10:46:17
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Dislocation
发表于 2025-3-26 13:57:01
1876-1682 on mechanism of barite-fluorite deposits. Summarizing the mineralization regularity of the deposit in this area of China provides a new insight and basis forthe study of similar types of deposits in the world..978-981-16-7564-5978-981-16-7562-1Series ISSN 1876-1682 Series E-ISSN 1876-1690
Perceive
发表于 2025-3-26 18:53:05
https://doi.org/10.1007/978-1-4020-6752-5adjacent areas occur in the Lower Ordovician Tongzi Formation and Fenxiang Formation. A small number of deposits of these formations and the Honghuayuan Formation occur in the first member of the Dawan Formation and the Baota Formation, with obvious characteristics of stratabound deposits.