The high-pressure metamorphic belts of Japan: A review
The high-pressure metamorphic belts of Japan: A review
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日本高压变质带：回顾
DOI：
10.1130/mem164-p365
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发表时间：
1986
期刊：
影响因子：
--
通讯作者：
S. Banno
中科院分区：
文献类型：
--
作者：
S. Banno
将日本群岛的高压变质岩划分为9个带或带：Tokoro带、Kamuikotan带、东Abukuma-Motai带、Hida Edge-Joetsu带、Sangun带、Sanbagawa带、黑尾川带、九州孤立区和八山带。Kamuikotan、东Abukuma-Motai、Hida Edge-Joetsu和KuroSegawa带与丰富的蛇纹岩有关。除了最后三个，所有的都是与低磷，高T的地体配对。Sangun和Sanbagawa带分别与低P和高T的Hida和Ryoke带配对。目前尚不清楚Kamuikotan区是否与日本群岛的任何低压地体配对。其他地体都很小，构造意义不确定。
High-pressure metamorphic rocks of the Japanese Islands are classified into 9 belts or zones: Tokoro, Kamuikotan, East Abukuma-Motai, Hida Marginal-Joetsu, Sangun, Sanbagawa, Kurosegawa, isolated area of Kyushu, and Yaeyama. The Kamuikotan, East Abukuma-Motai, Hida Marginal-Joetsu, and Kurosegawa zones are associated with abundant serpentinite. All but the last three are paired with low-P, high-T terranes. The Sangun and Sanbagawa belts are paired with the low-P and high-T Hida and Ryoke belts respectively. It is still not clear if the Kamuikotan Zone is paired with any low-pressure terrane in the Japanese Islands. The other terranes are small and of uncertain tectonic significance.