ore bodies

矿体

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矿体
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The whole-phase grade has been used to define ore bodies of a weathering-crust-type rare-earth deposit and to calculate its reserves.
The intrusion of alkali-syenite is considered to be the main factor of the ore bodies emplacement.
The occurrence of ore bodies is of great importance for the choice of the exploration methods.
With diverse shapes and different scale, the ore bodies are hosted along the contact belt between the intrusives and carbonate rocks.
This paper deals with the basic features, distribution pattern and association relation of the various ore bodies.
This model has been proved to be effective in the prognosis of blind ore bodies in certain gold ore districts and their surrounding areas.
Purple fluorites were deposited in acid environment of the early stage hydrothermal activity, and occurred nearest to ore bodies.
Some case studies indicate that the lateral trending of ore bodies has close relation to the dynamics during mineralization epoch.
Different ore bodies reflect different ore-controlling structures, different ore body sizes, and different rock ore occurrences.
Sulfide ore bodies are mainly composed of galena, sphalerite, calcite and minor amounts of pyrite and marcasite, with no quartz.
Ore mineralization is closely related with the faults, and the ore bodies in the control of the North East, North-West fault zone.
The Ore bodies are in conformity with the country rocks in attitude, occurring in bedded or bed-like form and forming synchronous folds.
Although there are 60 tin-bearing greisen veins, only a few of them form the main ore bodies.
Study of genetic relationship between dikes and gold ore bodies in Kubusu gold deposit in east Junggar .
The ore bodies are broadly distributed in simple layers, with stable occurrence, shallow depth and huge reserves.
Porphyry mineralization, occurred in the Silurian Period, finally formed ore bodies.
The ore bodies occur within or near the exocontact of intrusive rocks and above the hidden igneous rocks.
The ore bodies occur in bedded and stratoid forms and are stable along strike and direction of dip.
The ore bodies are stratiform or stratoid in the depth and vein form at the shallows, displaying an overpass pattern mineralization.
网络释义

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 …
更新时间：2025-04-26 17:57

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