نتایج جستجو برای: karst bauxite
تعداد نتایج: 5428 فیلتر نتایج به سال:
Two types of bauxite occur in the Jajarm Bauxite deposit, the first one is the hard bauxite and the other is the shaly bauxite or soft bauxite. The Al 2 O 3 content ranges from 30% to 60% and SiO 2 varies between 5% to 39%.The total tonnage is more than 22 million tons with a mean value of Al 2 O 3 content between 47% to 48% , SiO 2 around 10% and Fe 2 O 3 ranges between 6.95 to 27% . The Jajar...
Karst bauxite is a major source of aluminum and contains high concentrations trace elements such as Li, Ga, Sc, rare earth (REEs). It regarded potential non-conventional REE due to the increasing demand for REEs. This study provides new mineralogical geochemical evidence Lindai deposit in central Guizhou Province, aiming analyze genesis minerals reveal forms REEs occurring these deposits. The r...
The Miocene Climatic Optimum (MCO) represents a global warm period (approximately 17–14.7 Ma) interrupting long-term of Cenozoic cooling. To elucidate if bauxitization took place in southeastern European mid-latitude areas during the MCO, we studied section undated massive karst bauxite (Crveni Klanac, CK) central Dalmatia, Croatia, hosted Upper Cretaceous limestones and overlain by Sinj Basin ...
Karst flash flooding, identified as one of the hazards in karst terrains, is directly linked to the structure and hydraulic properties of karst aquifers. Due to the characteristics of flow within karst aquifers, characterized by a dual flow – diffuse flow within fissured limestone and conduit flow within karst conduits networks – flash flooding may be important in volume and dynamics. Such phen...
Iron Loss During Continental Weathering in the Early Carboniferous Period Recorded by Karst Bauxites
Abstract Significant iron (Fe) loss can occur during continental weathering and efflux to the ocean via runoff, historically affecting global Fe cycling marine ecosystems. Here, we report extremely low content in early Carboniferous (ca. 340 Ma) bauxites southwestern China. These were formed by redeposition of terrestrial soils along paleo‐continental margin western South China Plate warm clima...
Aluminium, the third most abundant element in the earth’s crust, occurs in nature in combination with silicon and oxygen (i.e. as aluminium silicate). When subject to tropical weathering, aluminium silicate may react to form aluminium hydroxide. Rock containing high concentrations of aluminium hydroxide is called bauxite. This rock is the usual starting material for the production of aluminium....
In this paper we present and elaborate one research example when bauxite was the main target of the investigation. During reprocessing and reinterpretation of the original data from the “Crvene stijene” locality near Jajce in Bosnia and Herzegovina, it was established that bauxite hanging wall and footwall rocks in fact represent an even more valuable mineral resource, as “dimension stone”. The...
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East of Shahindezh (south of West Azarbaidjan province), as a part of Irano-Himalayan karst bauxite belt, comprises discontinuous layers and lenses of bauxite, laterite, and kaolin within the Ruteh carbonate formation (Middle- Upper Permian). The XRD analyses show that the lateritic ores have rather simple mineralogy, and consist of hematite, boehmite, and kaolinite as major phases accompanied ...
biglar permo-triassic bauxite deposit is located in ~15 km northwest of abgarm, southwest of ghazvin province, west of central iran. it consists of 8 stratiform and discontinuous bauxite lenses lying along the contact of ruteh (permian) and elika (triassic) carbonate formations. petrographically, the bauxite ores exhibit collomorphic-fluidal, pseudo-breccia, pseudo-porphyritic, panidio-morphic-...
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