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ore bodies

网络矿体

ore bodies

ore bodies

ore bodies

矿体

...红山铜矿床、甘肃白银厂黄铁矿型铜矿床 2、矿体矿体 (Ore bodies) 呈层状、似层状、透镜状，多与地层整合产出，少数不 …

2

The whole-phase grade has been used to define ore bodies of a weathering-crust-type rare-earth deposit and to calculate its reserves .

一直以来，风化壳型稀土矿床均以全相品位来圈定矿体，计算全相储量。

3

The intrusion of alkali-syenite is considered to be the main factor of the ore bodies emplacement .

岩体侵入活动是导致工业矿体就位的主要因素。

4

The occurrence of ore bodies is of great importance for the choice of the exploration methods .

矿体产状对勘探手段的选择甚为重要。

5

With diverse shapes and different scale , the ore bodies are hosted along the contact belt between the intrusives and carbonate rocks .

矿体形态复杂，大小不一，主要赋存于中生代中性侵入体与中奥陶统碳酸盐岩接触带及附近。

6

This paper deals with the basic features, distribution pattern and association relation of the various ore bodies .

本文介绍了各种矿体的基本特征、空间展布、共生关系。

7

This model has been proved to be effective in the prognosis of blind ore bodies in certain gold ore districts and their surrounding areas .

构造叠加晕法在一些金矿区深部及其外围预测盲矿已取得了显著效果。

8

The molybdenum ore bodies favorite skarn, with molybdenite commonly enriched at the concentration of garnet, in dissemination or veinlets .

钼矿体多产于夕卡岩内，辉钼矿常于石榴石集中处富集，呈浸染状或细脉状。

9

Purple fluorites were deposited in acid environment of the early stage hydrothermal activity , and occurred nearest to ore bodies.

绿色、白色萤石在热液活动中 —晚期于中性介质中沉淀而成，距矿体较远；

11

The ore bodies were controlled by ductile shear metamorphic deformation belt , the genesis of the deposit is a superimposed . . .

矿体受韧性剪切变形变质带控制，矿床成因为变质热液与岩浆热液叠加的复合型。

12

The ore bodies are mainly controlled by the hypabyssal --ultrahypabyssal intrusive body and its inner or nearby fault-fissure system .

矿体主要受浅成超浅成侵入体及其内部和附近的断裂裂隙系控制。

13

Some case studies indicate that the lateral trending of ore bodies has close relation to the dynamics during mineralization epoch .

实例研究表明矿体的侧伏向与成矿期的动力学之间具有密切的成因联系。

14

Different ore bodies reflect different ore -controlling structures, different ore body sizes, and different rock ore occurrences.

不同的矿体形态反映不同的控矿构造，反映不同的矿体规模，反映不同的成矿岩体形态产状。

15

Subvolcanic dome consisting of complex and associated circular radial structures controls the distribution of gold ore bodies .

杂岩体构成的潜火山穹隆及伴生的环状放射状构造，控制着矿体的分布。

16

Sulfide ore bodies are mainly composed of galena , sphalerite , calcite and minor amounts of pyrite and marcasite, with no quartz .

矿石的矿物共生组合为闪锌矿方铅矿少量黄铁矿少量白铁矿方解石，不含石英。

17

Ore mineralization is closely related with the faults , and the ore bodies in the control of the North East , North-West fault zone.

矿体成矿作用与断裂构造密切相关，矿体受北东、北西断裂带控制；

18

The Ore bodies are in conformity with the country rocks in attitude, occurring in bedded or bed-like form and forming synchronous folds .

矿体产状一般与围岩一致，呈层状、似层状，并呈现同步褶皱。

19

Although there are 60 tin-bearing greisen veins , only a few of them form the main ore bodies .

共圈出含锡云英岩脉 60 余条，但主矿体却只有少数几条。

20

Uranium ore bodies are planar or lenticular in shape and under the control of the contact between gray sandstones and bleached sandstones .

铀矿体呈板状、透镜状，受漂白砂岩与灰色砂岩接触带控制。

21

22

Study of genetic relationship between dikes and gold ore bodies in Kubusu gold deposit in east Junggar .

东准噶尔库布苏金矿床岩脉与金矿成因关系的研究。

23

The ore bodies are broadly distributed in simple layers , with stable occurrence , shallow depth and huge reserves .

矿层主要呈层状、似层状，形态简单，产状稳定，埋藏浅，分布广，储量大。

24

Detailed research should be carried out when applying the model of the space distribution to predict the blind ore bodies at depth .

因此，应用此分带模式进行深部矿体预测时，应具体情况具体分析。

25

Porphyry mineralization , occurred in the Silurian Period , finally formed ore bodies.

晚期矿化发生于志留纪，使矿床最终形成。

26

Some large ore bodies in this environment at Selukwe Peak mine and elsewhere have been mylonitized almost completely .

在塞卢奎峰矿山等一些地方某些大的矿产在这种环境中，并几乎彻底被糜棱岩化。

27

The ore bodies occur within or near the exocontact of intrusive rocks and above the hidden igneous rocks .

金矿产于岩体外接触带及其附近和隐伏岩体上方。

28

The lamprophyres in Beiya gold district are veins formed during gold mineralization . They controlled the distribution of gold ore bodies.

北衙金矿区煌斑岩为成矿期脉岩，控制了金矿体的空间分布；

29

The ore bodies occur in bedded and stratoid forms and are stable along strike and direction of dip .

矿体呈层状、似层状产出，沿走向、倾向延伸比较稳定。

30

The ore bodies are stratiform or stratoid in the depth and vein form at the shallows , displaying an overpass pattern mineralization .

矿体在较深部呈层状、似层状而在浅部呈脉状，构成立交桥式矿化格架。

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