Pakistan is geographically situated in such a way that it consist of parts of two major and one minor plate namely
Indian plate
Eurasian plate
Arabian plate
Here Indian and Eurasian plates are major plates while Arabian plate is a minor plate which lies in the southern most side of Pakistan, while Indian plate is present on the eastern part and Eurasian plate includes the north western part of Pakistan. Therefore triple junction point is located within Pakistan (a point where three plate boundaries meet).
Pakistan is a host of several minor and five major faults which runs across it they are due to the previous tectonic events which occurred in this zone the major and most important event which resulted in the formation of the five major faults and is perhaps the reason of minor faults and is sill affecting the geology and tectonics of Pakistan is the famous Himalayan orogeny which itself formed as a result of Indian and Eurasian plate collision in about 20 million years ago because of the continental – continental collision .
Basically Indian plate which was situated within the Australian plate in gondwanaland and started moving towards north in a counter clockwise direction Neo Tethys Ocean was present between Eurasian and Indian plate a segment of this ocean started subducting beneath the Tethys ocean on its either sides/boundaries creating intra-oceanic island arcs due to the northward movement of Indian plate this arc collided with the southern Eurasia forming the continental-magmatic arc suture zone because of this collision folding thrusting occurred forming two major blocks Karakorum block and the kohistan ladakh arc (KIA) separated by MKT Main Karakorum Thrust. During the same time period rest of the Tethys ocean subducted beneath the Eurasian plate which afterwards caused the collision of Indian and Eurasian plate forming Himalayas this again resulted in the formation of thrust faults and fold the first major thrust fault which was formed here was the MCT (its branch in Pakistan is called MMT) this was north wards dipping later on after its formation stresses shifted southwards and another active fault called MBT (Main Boundary Thrust) was formed by the under thrusting of rocks beneath the MCT, Later on stresses shifted further southwards leading to the formation of SRT.