1) highly strained structural belt
强应变构造带
1.
The highly strained structural belts in some units of palaeo plate tectonics, products of subduction and collision of various scale plates in East Junggar, controlled the distribution of the majority of the endogenetic gold deposits and occurrences,turning into the most important gold metallogenic system in East Junggar.
东准噶尔强应变构造带形成于板块构造的特定部位 ,是不同级别板块俯冲、碰撞作用的产物 ,控制着该区大部分内生金矿的分布 ,并构成了该区最重要的金成矿系统 。
2.
Eastern Junggar highly strained structural belt is a product of plate collision.
东准噶尔强应变构造带是板块碰撞作用的产物 ,控制了金成矿带的分布 ,而金的矿化富集地段分布于强应变构造带与走向北北西的断裂交汇部位。
2) strong strain zone
强应变带
1.
It is helpful for our mapping objectively,dineating reasonablly the linear strong strain zone and weak strain domain, and revealing thd deformational and metamorphic history of Wudang Gr.
求文以1:5万凉水河镇幅、浪河镇幅区调资料为基础,阐述了武当山群的原生层理(So)、板劈理(S1B)、分异层理(S2C)和折劈理(S3Z)等面理的宏观及微观特征,探讨了其成生及演化关系,意义在于:客观地进行地质境图,合理地划分线状的强应变带与弱应变城,以揭示武当山群的变形变质及演化史。
3) Strong earthquake structure zone
强震构造带
4) tectonic strain
构造应变
5) tectonic transfer zone
构造变换带
1.
Relationship between tectonic transfer zones and petroleum accumulation in Banqiao Sag,Dagang Oilfield;
大港油田板桥凹陷构造变换带与油气富集
6) Altered tectonic zone
蚀变构造带
补充资料:椐椐强强
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