نتایج جستجو برای: carbonate replacement deposit
تعداد نتایج: 153195 فیلتر نتایج به سال:
Manganese deposits in the Early Carboniferous Baping Formation of central Guangxi, South China were formed Youjiang Basin on southern passive margin Block. Hosted Second Member Formation, manganese ore layers interbedded by thin-middle carbonate and silicified carbonate. Previous studies provide limited information about this deposit, sedimentary characteristics ores metallogenic mechanism are ...
In 1975, Social Security beneficiaries were given the option of having their monthly benefit payments sent directly to their banks through an electronic funds transfer system. Since then, beneficiaries have been enrolling in this program in rapidly increasing numbers. At the end of 1976, fewer than 5 million beneficiaries--14 percent of the total--were enrolled in the program. By the end of 198...
Parking Services [1] Parking permits are required to park on campus. Parking permits can be purchased online. Campus Map [2] The Campus map allows you to search for a location on campus by selecting a building or selecting a department name. Identification (ID) card Please visit Human Resources, 5th floor, South Tower, University Centre, to complete an ID application form. Your University of Gu...
Parking Permits [1] Parking permits are required to park on campus. Parking permits can be purchased online. Campus Map [2] The Campus map allows you to search for a location on campus by selecting a building or selecting a department name. Identification (ID) card Please visit Human Resources, 5th floor, South Tower, University Centre, to complete an ID application form. Your University of Gue...
X-ray powder diffraction and chemical analyses show that mammalian dental enamel apatite is an impure form of hydroxylapatite, Ca10(PO4)6(OH)2 (structure described in Elliott 1994). The major difference of enamel apatite from hydroxylapatite is in the presence of about 3 wt% CO3. Details of the crystallographic structures of carbonate-containing apatites (including minerals) are important becau...
The sulfuric acid speleogenesis (SAS) model was introduced in the early 1970s from observations of Lower Kane Cave, Wyoming, and was proposed as a cave-enlargement process due to primarily H2S autoxidation to sulfuric acid and subaerial replacement of carbonate by gypsum. Here we present a reexamination of the SAS type locality in which we make use of uniquely applied geochemical and microbiolo...
هدف مطالعه کنونی تعیین هنجارهای حاکم بر ترجمه ی آهنگهای کارتونها میباشد . به این منظور 30 آهنگ انگلیسی کارتونها و دوبله ی فارسی آنها انتخاب و بررسی شدند. ابتدا بر اساس مدل,low (2013) ترجمه آهنگها به سه دسته تقسیم شدند: 1) .song replacement (3 ,song adaptation (2 ,song translation سپس استراتژیهایی که مترجمین در جهت غلبه بر محدودیتهای ترجمه آهنگها به کار برده بودند بر اساس مدل ,low (2013) تعیین ش...
We recently showed that the production of elemental sulphur and calcium carbonate (CaCO3) from gypsum waste by thermally reducing the waste into calcium sulphide (CaS) followed by its direct aqueous carbonation yielded low-grade carbonate products (i.e. <90 mass% as CaCO3). In this study, we used the insight gained from our previous work and developed an indirect aqueous CaS carbonation process...
Pulverized limonite ore from a Pleistocene–Quaternary lake deposit and compact limonite ore from the Olistostrome member of the Javorik fl ysch formation, in the Southern Tomašica iron ore deposit, were investigated and compared with different types of siderite and ankerite, limestone and carbonate shale from the same location in order to determine their possible protolith. Two limonite types d...
This research analyzed the reservoir quality of Mfamosing Limestone with a view to classifying it as potential rock within Calabar Flank. Materials used in this are processed seismic data acquired around flank and well logs three wells (A, B, C) drilled at different periods study area, core mud log data. The procedure involved prospect identification mapping, structural stratigraphic analysis, ...
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