次生巖漿 的英文怎麼說
中文拼音 [cìshēngyánjiāng]
次生巖漿
英文
secondary magma-
The most important tectonothermal event in the ncc took place at ca. 1800 ma. the event was traditionally interpreted as the " luliang movement ", marking the finial cratonization of the ncc
華北陸塊最重要的一次構造-巖漿-變質活動發生在1800ma ，傳統上被稱之為「呂梁運動」 ，並作為華北克拉通基底穩定化的標志。Those two phases of conjugated shear joints are differ from each other in spatial distribution, which is a reflection of the spatial evolution of the fault zone. it can beinferredfrom the information about macrostructure, superimposed deformation of tectonites, paleotectonic stress field of joints and other related documents that there had been three stages of significant activity since zijingguan fault zone was activated. the first stage was about from middle juiassic to early cretaceous, when the fault zone activated left - laterally under nw - se striking transpression
宏觀構造組合特徵、構造巖變形疊加信息、節理的古構造應力場信息及前人區域資料表明，紫荊關斷裂帶自古生代末開始活化以來有三次主要構造活動：第一次是中侏羅世?早白堊世，在北西?南東向近水平擠壓作用下，斷裂左行壓扭性活動，控制太行山地區巖漿巖帶及與其相關的接觸交代型礦床的形成。It brings forward that the basic - superbasic cluster ( band ) related ni is variscan magmatic rock. it lies in the jin ping superficial fault unit ( also named " golden band " ) of subsidiary fracture unfold and wheel position of hong he " s profound fault and the marginal overgrowth band of yang zi platform
通過上述研究，認為該與鎳有關的基性-超基性巖群（帶）為華力西期巖漿巖，位於紅河深大斷裂舒展轉彎部位的次級斷裂上、揚子地臺邊緣增生帶的金平蓋層斷塊單元中（也稱「金鑲邊」帶中） 。
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