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The Duolanasayi gold deposit, 60 km NW of Habahe County, Xinjiang Uygur Autonomous Region, is a mid-large-scale gold deposit controlled by brittle-ductile shearing, and superimposed by albitite veins and late-stage magma hydrothermal solutions. There are four types of pyrite, which are contained in the light metamorphosed rocks (limestone, siltstone), altered-mineralized rocks (chlorite-schist, altered albite-granite, mineralized phyllite), quartz veins and carbonatite veinlets. The pyrite is the most common ore mineral. The Au-barren pyrite is present mainly in a simple form and gold-bearing pyrite is present mainly in a composite form. From the top downwards, the pyrite varies in crystal form from {100} and {210} {100} to {210} {100} {111} to {100} {111}. Geochemical studies indicate that the molecular contents of pyrite range from Fe1.057S2 to Fe0.941S2. Gold positively correlates with Mn, Sr, Zn, Te, Pb, Ba and Ag. There are four groups of trace elements: Fe-Cu-Sr-Ag, Au-Te-Co, As-Pb-Zn and Mn-V-Ti-Ba-Ni-Cr in pyrite. The REE characteristics show that the total amount of REE (ΣREE) ranges from 32.35×10 -6 to 132.18×10 -6; LREE/HREE, 4.466-9.142; (La/Yb)N, 3.719-11.133; (Eu/Sm)N, 0.553-1.656; (Sm/Nd)N, 0.602-0.717; La/Yb, 6.26-18.75; δEu, 0.628-2.309; δCe, 0.308-0.816. Sulfur isotopic compositions (δ 34S=-2.46‰--7.02‰) suggest that the sulfur associated with gold mineralization was derived from the upper mantle or lower crust. 相似文献
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Ping Shen Yuanchao Shen Tiebing Liu Guangming Li Qingdong Zeng 《Mineralium Deposita》2008,43(5):499-517
Integrated geological and geophysical investigations were carried out in 26 active mines in Northwestern China during the
period 2001–2006 to explore for hidden extensions of known ore bodies and to search for new mineralization. This paper presents
four case studies from northwest China: the Kuoerzhenkuoa volcanogenic hydrothermal gold deposit, the Nanjinshan breccia-associated
gold deposit, the Duolanasayi deposit, associated with a ductile–shear zone, and the Hulu magmatic Cu–Ni sulfide deposit.
In these studies, detailed mine-scale geological studies were carried out to determine the location and controls on ore formation.
Based on these investigations and a review of previous exploration data, genetic models for the deposits were evaluated, and
specific new targets were generated. These target areas were tested with surface geophysical surveys using the Stratagem EH4
system, a hybrid-source magnetotellurics (MT) method. Analysis of the data obtained in the surveys identified geophysical
target anomalies that were subsequently drilled. Many of these test holes demonstrate the presence of Au and Cu–Ni mineralization.
Evaluation of the geological models was crucial in developing conceptual targets as a basis for surface geophysical surveys.
These models established the most likely target areas where Au and Cu–Ni mineralization could occur, but they did not define
the limits or the geometries of the mineralized zones. Hybrid MT surveys played an important role in defining the location
of buried mineralized systems and in testing the validity of the conceptual targets. The resistivity cross-sections obtained
by imaging the MT data established the boundaries and geometries of the host rocks, including the distribution of lithology,
structures, alteration, and mineralization. The four case studies in this paper show how this integrated geological and geophysical
approach was used successfully to discover hidden mineral deposits.
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Ping ShenEmail: |
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1IntroductionTheDuolanasayigolddeposit,6 0kmNWofHabaheCountyinXinjiang ,issituatedonthenorth westernmarginoftheVariscianErtixorogenicbelt.Itisamedium largescalegolddepositcontrolledbythecoupledore formingprocessesinvolvingbrittle ductileshearing ,albititeve… 相似文献
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