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orogenic belt

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  • 网络造山带

orogenic beltorogenic belt
英-英网络释义

orogenic belt

造山带

地质专业英语词汇N-O ... orogenic 造山的 orogenic belt 造山带 orogenic cycle 造山旋回 ...

例句：
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Kalatongke Cu Ni deposit is of magmatic seperation type ore deposit occurring in orogenic belt far from craton.
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The structure of the orogenic belt in northern Taiwan could also be explained by a kinematic model of transpression.
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The uplifting of the Late Cretaceous was limited in the area of the Kuqa Depression and had no effect on the Tianshan orogenic belt.
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In the Late Devonian, the orogenic process was strong in the western part of the orogenic belt and formed n disintegration area.
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The Zhangbaling tectonic belt is a part of the Dabie orogenic belt and an outcrop area of the mid-upper crust of the belt.
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The Altai Hercynian orogenic belt in northern Xinjiang has experienced two stages (regional) metamorphism.
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Geochemical properties of the variolitic andesite from Susong in the Dabie orogenic belt, China .
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The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
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The Hexian County is located in the transitional area of the Yangtze block, the North China Block and the Dabie Orogenic Belt.
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Eastern section of Bogda orogenic belt is near the East Junggar orogenic belt.
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It is suggested that the confirmation of "Jiangnan orogenic belt" has been supported by full petrological evidences.
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They are one part of North China plate and the collision orogenic belt between North China plate and Yangtze Plate, respectively.
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NanzhaoFangcheng mineralization belt lies at the junction of North China plate and North Qinling orogenic belt.
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The north area of Weihe River is located in the joint of the Qilian-North Qinling orogenic belt.
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These stations distributed in three tectonic regions, which is Qinling orogenic belt, Weihe graben and Ordos block respectively.
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The quality of seismic data acquired from the south side of nappe structure in Micang-Daba mountain central orogenic belt is well improved.
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The Gonghe-Huashixia area is a key node of conjunction and transformation of the Central Orogenic Belt.
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During Triassic, this orogenic belt was peneplaned, and the basins parallel to orogenic belt were further developed.
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In China, Dabie-Sulu collisional orogenic belt develops the most well-exposed and largest in scale UHP metamorphic belt in the world.
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This is the first report of ferrogabbros in the Yanshan orogenic belt.

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