GENIE FOR DUMMIES

Over the Original collision with the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or more, remarkably metamorphosed, very deformed, and partially remelted in the Eocene Time period to sort gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and finally exhumed and uplifted

On top of that, the indole Main is substituted at R3 by using a carbonyl team that's also bonded into a napthalene moeity. Napthalene can be a bicyclic composition of two fused benzene rings. This carbonyl bridge of JWH-018 classifies it for a ketone. JWH-018 is definitely an analog of THJ-018, in which the Main indazole composition is substituted