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  2. Metasedimentary rock - Wikipedia

    en.wikipedia.org/wiki/Metasedimentary_rock

    In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment. Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be ...

  3. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    The Himalayas border the Indo-Gangetic Plain to the south, Pamir Mountains to the west in Central Asia, and the Hengduan Mountains to the east on the China–Myanmar border. From east to west the Himalayas are divided into 3 regions, Eastern Himalaya, Central Himalaya, and Western Himalaya, which collectively house several nations and states.

  4. Main Central Thrust - Wikipedia

    en.wikipedia.org/wiki/Main_Central_Thrust

    the Lesser Himalayan Sequence, which is mainly composed of low-grade Proterozoic metasediments to unmetamorphosed rocks, fringed by the Main Boundary Thrust and the Main Central Thrust; the Greater Himalayan Crystalline complex, which is mainly composed by high-grade gneiss and migmatite , fringed below by the Main Central Thrust and the South ...

  5. Metavolcanic rock - Wikipedia

    en.wikipedia.org/wiki/Metavolcanic_rock

    Metavolcanic rock is volcanic rock that shows signs of having experienced metamorphism. [1] In other words, the rock was originally produced by a volcano , either as lava or tephra . The rock was then subjected to high pressure, high temperature or both, for example by burial under younger rocks, causing the original volcanic rock to ...

  6. Carbonate–silicate cycle - Wikipedia

    en.wikipedia.org/wiki/Carbonate–silicate_cycle

    This figure describes the geological aspects and processes of the carbonate silicate cycle, within the long-term carbon cycle. The carbonate–silicate geochemical cycle, also known as the inorganic carbon cycle, describes the long-term transformation of silicate rocks to carbonate rocks by weathering and sedimentation, and the transformation of carbonate rocks back into silicate rocks by ...

  7. Plastiglomerate - Wikipedia

    en.wikipedia.org/wiki/Plastiglomerate

    Plastiglomerate could potentially form a marker horizon of human pollution on the geologic record. [1] [4] [5] [6] and may survive as future fossils. [2] [5] Plastiglomerate may also conceivably form in plastic-polluted regions affected by lava flows or forest fires. [1] [5] [6] They have been found on the surface as well as beneath the sand.

  8. Metasomatism - Wikipedia

    en.wikipedia.org/wiki/Metasomatism

    Metasomatism (from the Greek μετά metá "change" and σῶμα sôma "body") is the chemical alteration of a rock by hydrothermal and other fluids. [1] It is traditionally defined as metamorphism which involves a change in the chemical composition, excluding volatile components. [2]

  9. Paleogeography of the India–Asia collision system - Wikipedia

    en.wikipedia.org/wiki/Paleogeography_of_the_India...

    The dilemma is that the South Asian monsoon was believed to have originated from topographic rise of the Himalayas and Tibetan Plateau. The channel flow model predicts that the rise of Tibetan Plateau requires the presence of South Asian monsoon, which leaves the Himalayas as the only possible candidate responsible for initiating the monsoon ...