The discovery of bivalve fossils in Nimu area in Tibet and determination of related strata
-
-
-
图 1 含双壳化石地层地质剖面图(a)及地质简图(b)
1—第四系;2—麻木下组;3—构造岩石地层单位;4—渐新世似斑状正长花岗岩;5—渐新世—始新世似斑状二长花岗岩;6—始新世二长花岗岩;7—始新世花岗闪长岩;8—始新世石英闪长岩;9—始新世闪长岩;10—晚白垩世石英闪长岩;11—黑云斜长麻粒岩;12—透辉石大理岩;13—黑云斜长片岩;14—地质界线/逆冲断层;15—正断层/分层号
Figure 1. Geological section (a) and geological sketch map (b) of a bivalve fossil-bearing stratum
1-Quaternary; 2-Mamuxia Formation; 3-Tectonic rock stratigraphic unit; 4-Oligocene porphyritic syenite; 5-Oligocene-Eocene porphyritic monzonite; 6-Eocene monzonite; 7-Eocene granodiorite; 8-Eocene quartz diorite; 9-Eocene diorite; 10-Late Cretaceous quartz diorite; 11-Biotite plagioclase granulite; 12-Diopside marble; 13-Biotite plagioclase schist; 14-Geological boundary / thrust fault; 15-Normal fault / stratification number