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A greater gondwanaland.

A R Crawford

    Science (New York, N.Y.)
    |June 14, 1974
    PubMed
    Summary
    This summary is machine-generated.

    Ancient supercontinent Gondwanaland

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    Area of Science:

    • Geology
    • Paleogeography
    • Tectonic History

    Background:

    • Gondwanaland's maximum extent incorporated Tibet, the Tarim Basin, and northern China.
    • Tibet was situated as submerged continental crust between India and Western Australia.
    • The Himalayas originated from intracontinental processes.

    Purpose of the Study:

    • To delineate the paleogeographic configuration of Gondwanaland.
    • To understand the tectonic origins of the Himalayas and Tien Shan.
    • To clarify the position of Tibet and Tarim within Gondwanaland.

    Main Methods:

    • Paleogeographic reconstruction
    • Plate tectonic analysis
    • Geological mapping and stratigraphy

    Main Results:

    • Gondwanaland's maximum extent included key Asian landmasses.
    • Tibet's location indicates a submerged continental crustal setting.
    • The Himalayas formed through intracontinental deformation, not oceanic closure.
    • The Tien Shan mountains mark a former oceanic boundary of Gondwanaland.

    Conclusions:

    • The paleogeographic reconstruction clarifies the assembly of Gondwanaland.
    • Intracontinental processes were key to Himalayan orogeny.
    • The study refines our understanding of Asia's tectonic evolution within Gondwanaland.