1) mottled structure
斑点构造
1.
The mottled structure in the Dabeiwu area can be classified into syngenetic fragments and porphyroblasts, including seven types.
大背坞地区的斑点构造分为同生碎屑和变斑晶两大类共７种。
2) Spotted structures
斑点状构造
1.
Spotted structures are developed in ore-body and wall rock in Limin Gold Ore Belt .
斑点状构造是礼民金矿带矿化体岩石及围岩的显著特点,围绕中川岩体的北部、东部和南部成环带状于接触变质圈泥质岩石内发育,由岩体向外划分的红柱石亚带(Ⅲ)、(?)青石亚带(Ⅲ)、黑云母带(Ⅱ)和绿尼绢云母带(Ⅰ)中,其斑点构造的矿物组分由(?)青石+绢云母→黑云母+石英+黄铁矿。
3) murbruk structure
碎斑构造
4) dolomitized patches
云斑状构造
1.
The dolomitized patches were produced by early diagenetic dolomitization which preferentially began within Thalassinoides burrows and spread into the surrounding lime mud.
云斑状构造是早期白云石交代作用优先沿着痕迹化石Ｔｈａｌａｓｉｎｏｉｄｅｓ潜穴进行，然后向围岩扩散而形成的。
5) structural high
构造高点
1.
Relation of structural highs between overburden of salt and subsalt layers in Kelasu tectonic zone and petroleum geologic significance.;
克拉苏构造带盐上层与盐下层构造高点关系及石油地质意义
2.
Through data analysis on formation test,it is found out that the commercial producing formations are mainly distributed in four exploration wells (wells HL 1,HL 4,HL 8 and HL10) located at structural high.
川东北HL长兴组有着良好的油气潜能,通过对试油资料的分析,发现长兴组的工业产层主要分布在构造高点的HL1井,HL4井,HL8井,HL10井4口探井上。
6) structural knot
构造结点
1.
Due to strong inner-continental convergences since the Cenozoic, the Tethys in the Qinghai-Tibet Plateau presently has the structural kinematic features of two structural knots, three convergence boundaries and two great shear belts.
青藏特提斯是由5大地壳块体、3条板块缝合带经多期碰撞拼合而组成的复杂构造系统,由于新生代以来的强烈陆内汇聚作 用,现今主要表现为2个构造结点、3条汇聚边界和2大剪切带的构造运动学特征,边界的强烈汇聚与板内的强烈隆升、挤压剪切、 伸展剥离组成复杂而统一的动力学系统,具有厚壳和热壳特点。
补充资料：斑点
在一种颜色的物体表面上显露出来的别种颜色的点子。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条