Genesis of the Early Indosinian Darongshan Granitoid in South China: Response to the Subduction of the Eastern Paleo-Tethys Ocean

Figure 3

Field photographs: (a) Granite–porphyry intruded into sandstone formations; (b) granite–porphyry overlain by Late Mesozoic strata; (c) granite intruded into limestone formations; (d) granite intruded into Devonian Lianhuashan Formation strata (); (e) fault contact; (f) potassic granite with mafic microgranular enclaves (MMEs).

(a)

(b)

(c)

(d)

(e)

(f)