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Modern geologic ideas were introduced with the establishment of technical schools and the translation into Chinese of works by James D. Dana and Charles Lyell during the 1870s. Early in the twentieth century, foreign geology teachers were brought to China and Chinese students were sent to foreign countries to study geology.
The Yangtze plate, also called the South China block or the South China subplate, comprises the bulk of southern China.It is separated on the east from the Okinawa plate by a rift that forms the Okinawa Trough which is a back-arc basin, on the south by the Sunda plate and the Philippine Sea plate, and on the north and west by the Eurasian plate.
The Amurian microplate (or Amur microplate; also occasionally referred to as the China plate, not to be confused with the Yangtze plate) [citation needed] is a minor tectonic plate in the northern and eastern hemispheres.
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
Tectonic setting of the Tibetan Plateau showing main fault zones. The 1927 Gulang earthquake occurred at 06:32 a.m. on 23 May (22:32 UTC on 22 May). This 7.6 magnitude event had an epicenter near Gulang, Gansu in the Republic of China.
The rocks in the North China craton consist of Precambrian (4.6 billion years ago to 539 million years ago) basement rocks, with the oldest zircon dated 4.1 billion years ago and the oldest rock dated 3.8 billion years ago. [5]
He served the Chinese Ministry of Geology and Mining in giving training programs for Sedimentology (1979), Field Geology of Tibet (1980) and Plate Tectonics (1992). From 1983 to 1995, he assisted the Institute of Geology of the Chinese Academy of Sciences with the completion of a project on plate tectonics and to publish a new Geological Atlas ...
Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere.This type of tectonics is found at divergent plate boundaries, in continental rifts, during and after a period of continental collision caused by the lateral spreading of the thickened crust formed, at releasing bends in strike-slip faults, in back-arc basins, and on the continental end of ...