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  2. Geology of India - Wikipedia

    en.wikipedia.org/wiki/Geology_of_India

    Due to continental drift, the India Plate split from Madagascar and collided with the Eurasian Plate resulting in the formation of the Himalayas.. The earliest phase of tectonic evolution was marked by the cooling and solidification of the upper crust of the earth's surface in the Archaean Era (prior to 2.5 billion years) which is represented by the exposure of gneisses and granites especially ...

  3. M. S. Krishnan (geologist) - Wikipedia

    en.wikipedia.org/wiki/M._S._Krishnan_(geologist)

    Krishnan was born on 24 August 1898 in Tanjore, Madras Presidency.After school education in Tanjore, he continued his studies in St.Joseph's College, Tiruchirappalli. He graduated with B.A. Honours in geology from the Presidency College, Madras, in 1919, undertook post-graduate training and research with ARCS (Associate-ship of Royal College of Science) [2] Scholarship at Imperial College ...

  4. Geology of Indonesia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Indonesia

    The tectonics processes in Indonesia formed major structures in Indonesia. The most prominent fault in the west of Indonesia is the Semangko Fault or the Great Sumatran Fault, a dextral strike-slip fault along Sumatra Island (about 1,900 km). The formation of this fault zone is related to the subduction zone in the west of Sumatra.

  5. Palm-leaf manuscript - Wikipedia

    en.wikipedia.org/wiki/Palm-leaf_manuscript

    With the spread of Indian culture to Southeast Asian countries like as Indonesia, Cambodia, Thailand, Laos, and the Philippines, these nations also became home to large collections. Palm-leaf manuscripts called Lontar in dedicated stone libraries have been discovered by archaeologists at Hindu temples in Bali (Indonesia) and in 10th century ...

  6. Global Boundary Stratotype Section and Point - Wikipedia

    en.wikipedia.org/wiki/Global_Boundary_Stratotype...

    stratigraphy.org. Archived from the original on 2009-01-13. "Chart of The Global Boundary Stratotype Sections and Points (GSSP): chart". stratigraphy.science.purdue.edu. Archived from the original on 2022-06-30. "GSSP Table - All Periods". timescalefoundation.org. Archived from the original on 2023-11-30. "GSSPs and Continental drift 3D views".

  7. Chronostratigraphy - Wikipedia

    en.wikipedia.org/wiki/Chronostratigraphy

    Chronostratigraphy is the branch of stratigraphy that studies the ages of rock strata in relation to time. The ultimate aim of chronostratigraphy is to arrange the sequence of deposition and the time of deposition of all rocks within a geological region, and eventually, the entire geologic record of the Earth .

  8. Lameta Formation - Wikipedia

    en.wikipedia.org/wiki/Lameta_Formation

    The first fossils found in the Lameta Formation were discovered between 1917 and 1919. [2]The Lameta Formation was first identified in 1981 by geologists working for the Geological Survey of India (GSI), G. N. Dwivedi and Dhananjay Mahendrakumar Mohabey, after being given limestone structures–later recognised as dinosaur eggs–by workers of the ACC Cement Quarry in the village of Rahioli ...

  9. Brahmic scripts - Wikipedia

    en.wikipedia.org/wiki/Brahmic_scripts

    They are used throughout the Indian subcontinent, Southeast Asia and parts of East Asia. They are descended from the Brahmi script of ancient India and are used by various languages in several language families in South , East and Southeast Asia : Indo-Aryan , Dravidian , Tibeto-Burman , Mongolic , Austroasiatic , Austronesian , and Tai .

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