Electronic Resource

Geological and geochemical characteristics and genesis of Chenjiazhangzi cryptoexplosive breccia pipe gold deposit, Chifeng, Inner Mongolia.

التفاصيل البيبلوغرافية
العنوان: Geological and geochemical characteristics and genesis of Chenjiazhangzi cryptoexplosive breccia pipe gold deposit, Chifeng, Inner Mongolia.
المؤلفون: She Hong-Quan, Feng Cheng-You, Li Da-Xin, Meng Li-Jun, Wang Qi., Wang Zhong, Zhang De-Quan, Zhang Gui-Lan
نوع الوثيقة: Electronic Resource
مستخلص: The breccia pipe has been intensely altered and shows apparent alteration zoning, with Au mineralisation closely related to silication and adularisation. Electrum is the dominant mineral and mainly occurs in arsenopyrite. The primary mantle-normalised rare earth and trace element patterns of the breccia show enrichment of LREE and K and depletion of Eu, Ti, Sr, Ba, Th, U, in conformity with the features of non-mature normal arc granites on the continental margin. The homogenisation temperatures of fluid inclusions in quartz indicate that Au mineralisation took place mainly at temperatures of 150-180 degrees C and 225-390 degrees C. The deposit is of the epithermal-mesothermal type and was formed in the Early Yanshanian period.
The breccia pipe has been intensely altered and shows apparent alteration zoning, with Au mineralisation closely related to silication and adularisation. Electrum is the dominant mineral and mainly occurs in arsenopyrite. The primary mantle-normalised rare earth and trace element patterns of the breccia show enrichment of LREE and K and depletion of Eu, Ti, Sr, Ba, Th, U, in conformity with the features of non-mature normal arc granites on the continental margin. The homogenisation temperatures of fluid inclusions in quartz indicate that Au mineralisation took place mainly at temperatures of 150-180 degrees C and 225-390 degrees C. The deposit is of the epithermal-mesothermal type and was formed in the Early Yanshanian period.
مصطلحات الفهرس: 2005, ARSENOPYRITE, BRECCIA DEPOSITS, CHENJIAZHANGZI, CHINA, ECONOMIC GEOLOGY, ELECTRUM, EPITHERMAL DEPOSITS, FLUID INCLUSIONS, GEOTHERMOMETRY, GOLD, HYDROTHERMAL ALTERATION, HYDROTHERMAL DEPOSITS, INNER MONGOLIA, ISSUE063, MINER. DEPOSITS, MINERAL DEPOSITS, MINERAL ZONING, ORE GENESIS, TRACE ELEMENTS, text
URL: http://worldcat.org/search?q=on:UKMMM+https://icon.iom3.org/cgi-bin/koha/oai.pl+DCG_ENTIRE_REPOSITORY+CNTCOLL
الاتاحة: Open access content. Open access content
ملاحظة: und
Other Numbers: UKMMM oai:icon.iom3.org:93525
1309227097
المصدر المساهم: INSTITUTE OF MATS MINERALS & MINING
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رقم الانضمام: edsoai.on1309227097
قاعدة البيانات: OAIster