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

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

    At the suggestion of Cyril S. Fox of the Geological Survey of India (GSI) he decided to work on a book on Indian stratigraphy. This resulted in the publication of Geology of India and Burma in 1943 and the Introduction to Geology of India in 1944. The first book has gone through 6 editions and has also been translated into Russian.

  3. 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 ...

  4. Intertrappean Beds - Wikipedia

    en.wikipedia.org/wiki/Intertrappean_Beds

    Amarkantak Group or Mandla Province (age: early Paleogene, ~64.5 mya ... Western Ghats-Central Indian Volcanic Province (WVP) (age ... Stratigraphic position ...

  5. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    In the Late Cretaceous (84 Ma), the Indian plate began its very rapid northward drift covering a distance of about 6000 km, [6] with the oceanic-oceanic subduction continuing until the final closure of the oceanic basin and the obduction of oceanic ophiolite onto India and the beginning of continent-continent tectonic interaction starting at ...

  6. 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.

  7. Tectonic evolution of the Aravalli Mountains - Wikipedia

    en.wikipedia.org/wiki/Tectonic_evolution_of_the...

    The Aravalli Mountain Range is a northeast-southwest trending orogenic belt in the northwest part of India and is part of the Indian Shield that was formed from a series of cratonic collisions. [1] The Aravalli Mountains consist of the Aravalli and Delhi fold belts, and are collectively known as the Aravalli-Delhi orogenic belt.

  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. Dharwar Craton - Wikipedia

    en.wikipedia.org/wiki/Dharwar_Craton

    The location map of the Dharwar Craton. The shaded area represents the Dharwar Craton. Generated from GeoMapApp (Ryan et al., 2009). [1]The Dharwar Craton is an Archean continental crust craton formed between 3.6-2.5 billion years ago (), which is located in southern India and considered the oldest part of the Indian peninsula.

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