用mineralization造句子，“mineralization”造句

The source rocks are mafic volcanic rocks in the greenstone belt. The mineralization fluids are mainly metamorphic hydrothermal fluids. Middle Proterozoic is the main mineralization period.

The copper mineralization in Yueshan district of Anhui Provomce is typical of the Middleand Lower Reaches of the Yangtze River area, an important mineralization belt in China.

Middle north margin of North China platform is important concentration area of gold mineralization in China.

It is believed that there is a second mineralization location and new mineralization type in the depth of the mine with molybdenum (gold) polymetallic ore potential of porphyry series.

Further studies indicate that mineralization has intimate relationship with magmatic fractional crystallization, fluid boiling and fluid mixing.

This paper focused on the study of the most optimal geochemical interfaces controlling the mineralization and location of a 'xi gold deposit.

The gold contents of the altered fractured zone has been studied and the relation of gold mineralization with alteration types identified.

It is located in north part and west flank of the Panxi rift and belongs to the western sub-belt of REE mineralization in the west of Mianning region.

There were few reports about the south part of this gold belt. Based on the mineralization conditions and the data we have obtained, the author thinks this is a gold region we must pay attention to.

Poorly exposed mineralization is almost certain to be overlooked.

The Mineralization Preferentiality so called means that the super large and large deposits are located at special places with specific conditions of mineralization.

The mineralization type of Shaungqishan gold deposit has been divided into quartz vein and alteration type.

According to the synthetic analyses of various factors there is no prospect of uranium mineralization in the ancient terrain.

This area is the geochemical one with high copper background value and has the favourable condition for copper mineralization.

According to the study on ore-controlling role of subvolcanic rock, the authors think the calcium-alkali and intermediate acid subvolcanic rocks are important conditions for mineralization.

It is located in the west flank of the Panxi rift, but the REE mineralization was developed in the postrift stage based on the isotopic ages and the geological environment.

Carbonatization and greisenization are closely related to sn-w mineralization.

Xiongershan area is one of the major concentration areas of gold mineralization in western Henan.

This, with all available information on topography, primary and secondary mineral dispersal, helps to locate the mineralization.

The mineralization of gold ore and gold mineralized points round the rock bodies have a relation with granite body in Sanguliu.

There is a special relationship of gold mineralization to lead zinc mineralization.

Tongshi is a new type of ore field discovered recently with multi-mineralization types recognized. Crypto-explosion breccia Au mineralization is the major one.

REE geochemistry of silicated quartz reflects intensity and multiple epochs of gold mineralization in Wulonggou gold ore area.

The gold mineralization region is located in the margin of the Gongguan - Huilong Hg-Sb ore belt in the southeast end of the Indosinian miogeosyncline folding belts of the southern Qinling mountains.

Then cyclic stretching inhibited differentiation and mineralization of osteoblasts at all loaded time.

With the buried glass filter paper bag method a field experiment was carried out in a tobacco field to study mineralization of green manure and its effect on tobacco leaf quality.

Quartz diorite-porphyrite body is large in scale, and closely related with Cu mineralization.

The gold mineralization district of Fuxing-Duhuangling mineralization district is relative to the activity of Mesozoic volcanic magma.

The heating from the asthenosphere on the crust subsequently resulted in the intensive magmatism, mineralization, and widespread development of extensional structures in eastern China.

The formation of BIF hosted gold deposits in Wutai mountain area involves two different mineralization processes:primitive mineralization process and superimposed mineralization process.