The geology of Himachal Pradesh is dominated by Precambrian rocks that were assembled and deformed during the India-Asia collision and the subsequent Himalayan orogeny. The Northern Indian State Himachal Pradesh is located in the Western Himalaya (Fig. 1). It has a rugged terrain, with elevation ranging from 320m to 6975m. Rock materials in the region are largely from the Indian craton, and their ages range from the Paleoproterozoic to the present day. It is generally agreed that the Indian craton collided with Asia 50-60 million years ago (Ma). Rock sequences were thrust and folded immensely during the collision. The area has also been shaped by focused orographic precipitation, glaciation and rapid erosion.
Useful Links Geological time scale Related Disciplines Portal
Major tectonic units The elevation of Himachal Pradesh increases from SW to NE, and the orogenic materials making up this area also vary in the same direction. There are 5 major tectonic units in the form of fault-bounded NW-SE trending belts (Fig. 2). From SW to NE they are named the Indo-Gangetic Plain, Sub-Himalayan Sequence, Lesser Himalayan Sequence, Greater Himalayan Crystalline complex and Tethyan Himalayan Sequence (Fig. 2, 3).
The Indo-Gangetic Plain represents a recent, active foreland basin which comprises alluvial sediments derived from the Himalaya. The Sub-Himalayan Sequence mainly represents sediments deposited in the foreland basin during Miocene time. The Lesser Himalayan Sequence is a unit emplaced before the mountain-building processes. The Greater Himalayan Crystalline complex represents a high-grade unit moved towards SW from the hinterland. The Tethyan Himalayan Sequence represents strata deposited in the former passive margin in the Northern edge of Indian plate.
Indo-Gangetic Plain The Indo-Gangetic Plain (IGP), located at the southwestern fringe of the state, is an alluvial plain composed of sediments eroded from the Himalayan rocks. This area is an active depocenter that receives high sediment flux from the nearby major rivers. For instance, a high average erosion rate of 1.8 mm/yr has been reported in the frontal Sutlej's Himalayan catchment, contributing to large sedimentation load. Below the Indo-Gangetic Plain lies the generally undeformed Indian Craton strata. All of them are bounded by the Main Frontal thrust (MFT) at the northeast side.
Sub-Himalayan Sequence The Sub-Himalayan Sequence, also named the Siwalik Group, is dominated by Paleocene to Pliocene sedimentary layers. Sediments have a similar origin as those in the Indo-Gangetic Plain. However, sedimentation events started prior to the India-Asia collision and continued until late Miocene, and the depositional environment changed from shallow marine to continental. + StratigraphyAgeUnitLithologyDeposition environmentPleistocene-Miocene (11-7Ma)Siwalik FormationSandstone, conglomerate, siltstoneContinentMiocene (20-13Ma)Dharamsala FormationGray sandstone, siltstone, shale, calicheContinentLatest Paleocene-Middle EoceneSubathu Formationlimestone, shale, minor fine-grained sandstoneShallow marineLate Cretaceous-PaleoceneSingtali Formationlimestone, minor quartz areniteShallow marine
Two sub-groups have been identified, including the Paleocene to Eocene shallow-marine deposits and the Miocene to Pliocene continental deposits. The Singtali and Subathu Formation made up the older sub-group while the Dharamsala and Siwalik Formation made up the younger one. Separating the two is an Oligocene unconformity. It has been suggested that there was a period of non-deposition during the Oligocene due to temporary uplifting of the Indian continent. At that time, the area rose above sea level. Detachment of the Indian oceanic slab might have induced mantle upwelling, or a forebulge might have developed due to the downward slab-pull.
The Sub-Himalayan Sequence is thrust southwestward in the rate of 10±6 mm/yr along the Main Frontal thrust during the Quaternary. Within the sequence, rocks have been thrust and accreted vastly, forming the Sub-Himalayan Thrust Zone in the southwest Himachal Pradesh (Fig. 3). The unit is bounded by the Krol thrust and Tons thrust on top.
Lesser Himalayan Sequence (LHS) The Lesser Himalayan Sequence dominantly consists of metasedimentary rocks, metavolcanic rocks and augen gneiss. Strata were deposited as detrital sediments during Paleoproterozoic to Cambrian and later metamorphosed into greenschist and amphibolite facies rocks. This sequence is bounded by the Main Central thrust on top and can be sub-divided into 4 units. + StratigraphyAgeUnitLithologyNoteNeoproterozoic-lower CambrianOuter Lesser HimalayaTal Formation Krol Group
Shimla Group
Basantpur Formation (Mandhali)sandstone, siltstone, dolomite, limestone and shaleexposed at the south, southeast part of the statePaleoproterozoic-NeoproterozoicParautochthonDeoba Group Damtha Groupsiliciclastic and carbonate rocks exposed at the Uttarkashi and Narkanda Half-Windows part of the Inner Lesser HimalayaPaleoproterozoicBerinag Groupsericitic quartz-arenite with metabasalt intrusion rocks were metamophosed under a greenschist facies condition part of the Inner Lesser HimalayaPaleoproterozoicMunsiari GroupWangtu Jeorigranitic augen gneiss paragneiss, mica schist the Munsiari Group is also named Lesser Himalayan Crystalline Sequence (LHCS) experienced amphibolite facies metamorphism between 11 and 6 Ma (Miocene) exposed in tectonic windows (Uttarkashi and Kullu Window)
Greater Himalayan Crystalline Complex (GHC)
The Greater Himalayan Crystalline complex, also known as the High Himalayan Crystalline Sequence, is composed of high-grade metamorphic rocks aged between Paleoproterozoic and Ordovician. Over the 4.5–8 km thick layer, paragneiss, schist and orthogneiss are observed. Leucogranites are found to be concentrated at the uppermost part of this unit. Metamorphic grade of rocks increases upsection, with staurolite, kyanite, sillimanite and migmatite zones superimposed gradually. The crystalline complex had experienced peak metamorphic condition of 750 °C, 8kbar at around 23Ma.
The crystalline complex is bounded by the Main Central thrust at the base and South Tibet detachment on top. Consensus has not been reached regarding how the Greater Himalayan Crystalline Complex was emplaced to the orogen. Moreover, the anomalous extensional movement along the South Tibet detachment has intrigued many researchers.
South Tibet Detachment (STD) The South Tibet detachment lies between the Greater Himalayan Crystalline complex and the Tethyan Himalayan Sequence (Fig. 3). Alternating top-to-southeast and top-to-northwest shear directions have been identified by various ductile shear fabrics along the South Tibet Detachment. It has been suggested that in Himachal Pradesh, the South Tibet detachment is folded and overturned with the Phojal Anticline and joins the Main Central thrust at the southwest side. While some believe the South Tibet Detachment joins the Main Central thrust down-dip, or the two faults being parallel to each other (Fig.6).
Tethyan Himalayan Sequence (THS) + StratigraphyUnitNoteSedimentary RocksGiumal-Chikkim succession Tandi Group
Thaple-Muth-Lipak succession
Parahio Formation
Haimanta Group consists of sedimentary and low-grade metasedimantary rocks deposited at the northern boundary of the Indian continentIgneous RocksEarly Paleozoic granitoids Neoproterozoic granite
Baragaon granitic gneissemplaced in Cambrian-Ordovician, peraluminous with mafic enclaves ca. 830Ma
ca. 1850Ma The Tethyan Himalayan Sequence comprises Neoproterozoic to Cretaceous, fossiliferous sedimentary strata interlayered with Paleoproterozoic to Ordovician igneous rocks. At the base of this unit, Baragaon granitic gneiss having an age of 1840 Ma has been identified. Unlike the Greater Himalayan Crystalline complex in this region, metamorphic grade of rocks decreases upsection across the sequence. It is mostly bounded by the Indus-Tsangpo Suture at the northwest side and the South Tibet Detachment at the base. However, at the western part of Himachal Pradesh (longitude <77°E), the Main Central thrust and Lesser Himalayan Sequence rocks lies right beneath the Tethyan Himalayan Sequence.
The Tethyan Himalayan Sequence covers a large area of the Himachal Pradesh, since it overthrust the Lesser Himalayan Sequence, Greater Himalayan Crystalline Complex and the Sub-Himalayan Sequence successively during the Cenozoic.
Development of the thrust wedge Crustal materials of Himachal Pradesh were emplaced to the present position in response to the collision between the Indian and Asian continents. As collision proceeds, rocks are shortened and absorbed by subduction, thrusting and erosion. A portion of crust has been recycled to the mantle by subduction and slab break-off. The two colliding blocks have been rubbing against each other. Materials from the Indian Plate were scraped off by the Asian Plate. Both Indian and Asian sourced rocks were accumulated and piled up to form a thrust wedge (Fig. 4).
Rock units are stacked up and deformed by:
Frontal accretion — At the frontal part of thrust wedge, new faults propagate forward due to the compressive force. Rocks at the footwall are scraped off and become part of the hanging wall. This process repeats forming slices of rocks in the foreland basin (Fig. 5). Imbricate fans can be found in the Sub-Himalayan Sequence (Fig. 3). Underplating — Rock units are thrust and piled up section by section (Fig. 5). At the middle part of the thrust wedge, the Lesser Himalayan Sequence started to develop thrust horses and antiformal stacks at depth since 5.4Ma. Out of sequence faulting — The Munsiari thrust as the out-of-sequence thrust was developed recently from the Himalayan sole thrust. It truncated the Main Central thrust in this area.
These processes may have occurred simultaneously at different parts of the thrust wedge due to strong strain partitioning.
Assembly of the tectonic units There are mainly three different models explaining how the major tectostratigraphic units in Himachal Pradesh came together in Cenozoic (Fig. 6). The main controversy surrounds how the Greater Himalayan Crystalline complex was emplaced.
Wedge extrusion model In this model, the Main Central thrust and the South Tibet detachment join down-dip, enveloping the Greater Himalayan Crystalline complex. During early Miocene (23-17Ma), the Greater Himalayan Crystalline sequence was exhumed and verged southwestward with the activation of the Main Central thrust, leaving the surrounding sequences behind. A normal sense of movement was therefore created at the South Tibet detachment.
At the frontal part of the orogen, sustained crustal thickening might have increased loading locally. Substantially, the vertical stress exceeded the horizontal compressive stress. Maximum stress orientation was rotated and a normal fault was formed. In addition, the elevation of the Indian foreland might have surpassed that of Southern Tibet. Therefore, gravitational collapse and backsliding of crustal materials (Tethyan Himalayan Sequence) occurred.
Channel flow model In the channel flow model, the Greater Himalayan Crystalline complex was derived from Tibetan protolith instead of Indian protolith. The Main Central thrust and South Tibet detachment are sub-parallel to each other like channel walls. Initially, hot crustal melt was formed at middle to lower crust beneath the Tibetan Plateau. In the Eocene to Oligocene, the low-viscosity materials migrated southward between the Tethyan Himalayan Sequence and Lesser Himalayan Sequence. Later during early to middle Miocene, the upper crust in front of the channel flow was weakened by focused denudation. The Greater Himalayan Sequence is then exhumed to the modern position.
Tectonic wedging model