Typomorphic characteristics of main minerals from laowangzhai gold deposit , western yunnan
2.
The typomorphic character of quartz in jinchanggou gold deposit and it s application , jilin
3.
Mineralogical typomorphic characteristics of stibnite in the xikuangshan antimony deposit , hunan province
4.
Compared with other kinds of ore deposits , zinc - tennantite is a kind of typomorphic mineral in the altai mineralization province and is useful for the exploration of volcanogenic massive sulfide deposits
5.
By study hongyan deposit on minerogenetic and geological background , mineral constituent , rock alteration , rare - earth element , isotope and typomorphic feature of sulpurization mineral , we made a conclusion that the feature of haongyan is deposition - rebuilding desposit
6.
There are intensive structural and magmatic hydrothermal movement with obvious zonal surface shape alterations , which are demonstrated by silicified function , sericitization , potassium , epidotization , hornstone , etc . the ore structural fabric mainly behaves in form of filling action with minerals such as pyrite , chalcopyrite , salenite , blende and electrum , which typomorphic feature shows a hypothermal pattern of metallogeny
7.
It is difficult to conform the derivations of the native heavy minerals , so the author assumes corresponding procedures as follows to accomplish the research task : firstly , according to the composition typomorphic peculiarities of minerals deriving from mantle , the author selected a part of minerals as preliminary reseach objects from the native heavy minerals and then further investigate the mantle ones and their host rocks in two ways : one is the method of comparation with the corresponding minerals of rocks deriving mantle in the research field and other places ; anorther is the method of multivariate statistical analysis
8.
That offer very valuable referential material for future searching mineral . in recent years , many deposits were confronted with reserves crisis in yuebei region . so we studied the typomorphic feature of pyrites , galenite , sphalerite for deposit of yuebei region , and sum up the genesis of deposit and mineral and reseaching typmorphic feature , these have important value to forecast the deepth of deposit and reaserch the outside of deposit
9.
Based on the variation of light / heavy mineral components of sedimentary rocks , the typomorphic characteristics of various debris , the cathodoluminescence color of quartzes , the direction of paleocurrent and the extension of sedimentary facies , two source direction of the studied area in carboniferous and permian can be recognized , one is in bayanwusu , wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos , another is alashan area in the northwest margin of ordos
10.
In the course , the condition and the process of forming and changing of minerals , the typomorphic features of minerals , the characteristics of the distribution and the evolution of minerals and their paragenetic associations in the period and the space , the methods of mineral analyses and research , the geological thermometers and the geologicial barometers of minerals , mineral paragenetic associations and paragenesis analyses will be introduced , and the magnificent and the microscopic genetic characteristics of pyrite , quartz , garnet , pyroxene , amphibole , mica , feldspar , and other minerals will be dealt with particularly
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