安徽铜陵—繁昌地区深部成岩成矿作用探讨——来自综合地球物理探测的制约

王云云, 兰学毅, 郭冬, 张莎莎, 丁文祥, 陶龙, 张慧杰, 张媛媛, 叶林, 尤淼

Diagenesis and mineralization in Tongling and Fanchang areas, Anhui Province: Constrains from the integrated geophysical exploration study

WANG Yun-Yun, LAN Xue-Yi, GUO Dong, ZHANG Sha-Sha, DING Wen-Xiang, TAO Long, ZHANG Hui-Jie, ZHANG Yuan-Yuan, YE Lin, YOU Miao

图4 铜陵隆起区东部—繁昌盆地廊带1线地质—地球物理综合模型 1—第四系;2—白垩系上统赤山组;3—白垩系下统蝌蚪山组;4—白垩系下统赤沙组;5—白垩系下统中分村组;6—三叠系;7—二叠系中上统;8—石炭系—二叠系下统;9—泥盆系—志留系下统高加边组;10—奥陶系—寒武系;11—花岗闪长岩;12—花岗岩;13—花岗斑岩;14—花岗闪长斑岩;15—推断高密度体;16—逆断层;17—正断层

Fig.4 Geological-geophysical synthesized model of No. 1 section in Tongling and Fanchang region 1—Quaternary; 2—upper Cretaceous Chishan formation; 3—lower Cretaceous Kedoushan formation; 4—lower Cretaceous Chisha formation; 5—lower Cretaceous Zhongfencun formation; 6—Triassic; 7—Upper-middle Permian; 8—lower Carboniferous-Permian; 9—Devonian-lower Silurian Gaojiabian formation; 10—Ordovician-Cambrian; 11—granodiorite; 12—granite; 13—granitic porphyry; 14—granodioritic porphyry; 15—inferred high-density body; 16—reverse fault; 17—normal fault