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3 铜陵隆起区东部—繁昌盆地TL11-05线反射地震偏移剖面(据吕庆田等,2012修改)[24] 1—主要断裂;2—断裂;3—白垩系盆地底界;4—正断层;5—逆断层;6—盖层与基底之间滑脱面;7—中、下地壳之间滑脱面;Pt—元古宇基底地层;Pz—古生代地层;K-N—白垩-新近系

Fig.3 Reflection seismic profile No. TL11-05 line in the Tongling-Fanchang region(Modified after Lyu et al., 2012)[24] 1—main fault; 2—fault; 3—lower boundary of the Cretaceous basin; 4—normal fault; 5—reverse fault; 6—the detachment between basement and overlying strata; 7—the detachment between middle and lower crust; Pt—Proterozoic strata; Pz—Paleozoic strata; K-R—Cretaceous to Neogene