Paleogeographic maps of the Japanese Islands: Plate tectonic synthesis from 750 Ma to the present
Paleogeographic maps of the Japanese Islands: Plate tectonic synthesis from 750 Ma to the present
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DOI：
10.1111/j.1440-1738.1997.tb00043.x
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发表时间：
1997-03-01
期刊：
影响因子：
1.5
通讯作者：
Terabayashi, M
中科院分区：
文献类型：
--
作者：
Maruyama, S;Isozaki, Y;Terabayashi, M
从板块构造的角度，新编制了日本诸岛自750~700 Ma诞生至今的一系列古地理图。该系列由20幅地图组成，涵盖了日本大地构造演化中的所有重大事件。包括扬子克拉通裂解大陆边缘的日本诞生(约750-700 Ma)、大陆边缘由被动向活动的构造反转(约500 Ma)、古生代海山和大洋高原碎屑的增生生长(约480-250 Ma)、中朝与扬子的碰撞(250-210 Ma)、中、新生代的增生生长(210 Ma-今)，包括白垩纪成对变质带的形成(90 Ma)，以及中新世背部(25-15 Ma)，这些都是将日本作为一个岛屿分开的日本海的打开。
A series of paleogeographic maps of the Japanese Islands, from their birth at ca 750-700 Ma to the present, is newly compiled from the viewpoint of plate tectonics. This series consists of 20 maps that cover all of the major events in the geotectonic evolution of Japan. These include the birth of Japan at the rifted continental margin of the Yangtze craton (ca 750-700 Ma), the tectonic inversion of the continental margin from passive to active (ca 500 Ma), the Paleozoic accretionary growth incorporating fragments from seamounts and oceanic plateaux (ca 480-250 Ma), the collision between Sino-Korea and Yangtze (250-210 Ma), the Mesozoic to Cenozoic accretionary growth (210 Ma-present) including the formation of the Cretaceous paired metamorphic belts (90 Ma), and the Miocene back-are opening of the Japan Sea that separated Japan as an island are (25-15 Ma).