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1 安徽铜陵隆起区东部—繁昌盆地地质简图 1—第四系;2—白垩系;3—三叠系;4—二叠系;5—石炭系;6—泥盆系;7—志留系;8—火山岩;9—闪长岩;10—花岗岩;11—粗面安山玢岩;12—花岗斑岩;13—正长斑岩;14—闪长斑岩脉;15—辉绿斑岩脉;16—断层;17—推断主要断裂;18—廊带1线及MT剖面位置;19—收集的地震剖面位置

Fig.1 Location magnetotelluric measurement points and seismic section in the Tongling-Fanchang geological map 1—Quaternary;2—Cretaceous;3—Triasic;4—Permian;5—Carboniferous;6—Devonian;7—Silurian;8—volacanic rock;9—diorite;10—granite;11—trachylotic andesitic porphyry;12—granitic porphyry;13—syenitic porphyry;14—dioritic porphyry dyke;15—diabase prophyry dyke;16—fault;17—inferred main faults;18—location of No.1 line and MT section;19—location of the collected seismic section