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Titlebook: Bitumens in Ore Deposits; John Parnell,Henryk Kucha,P. Landais Book 1993 Springer-Verlag Berlin Heidelberg 1993 Bitumen.Hydrocarbon.Kohlen

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發(fā)表于 2025-3-21 19:48:21 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Bitumens in Ore Deposits
影響因子2023John Parnell,Henryk Kucha,P. Landais
視頻videohttp://file.papertrans.cn/189/188910/188910.mp4
學(xué)科分類Special Publication of the Society for Geology Applied to Mineral Deposits
圖書(shū)封面Titlebook: Bitumens in Ore Deposits;  John Parnell,Henryk Kucha,P. Landais Book 1993 Springer-Verlag Berlin Heidelberg 1993 Bitumen.Hydrocarbon.Kohlen
Pindex Book 1993
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Nomenclature, Classification, Characterization, and Genesis of Natural Solid Bitumen (Migrabitumen)tites (gilsonite, glance pitch, and grahamite), wurtzilite, albertite, and impsonites (epi-, meso- and cata-impsonite). In a genetic sense there are two main groups with ozocerite alone in one group and all the other migrabitumens in the other. Ozocerite is formed mainly from terrestrial source mate
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Transmission Electron Microscopy of Carbonaceous Matter in Precambrian Shungite from Karelia USSR). Its chemical structure differs considerably in comparison with other types of solid bitumen. Structural inhomogeneity is a characteristic feature of this carbonaceous matter. The structure of shungite is a result of some process which oxidized primary organic matter of probably algal origin,
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發(fā)表于 2025-3-22 11:11:48 | 只看該作者
Interpretation of Thermal Mesophase in Vanadiferous Bitumens from Upper Proterozoic Lava Flows (Míto, which are similar to poorly ordered graphite, show a marked mosaic and areal anisotropy typical of thermal mesophase that develops during industrial coking processes. The isotopic composition of the bitumen carbon (X δ.C –30.1‰) is within the range typical of organic carbon in the adjacent sedi-me
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Hydrocarbons and Gold Mineralization in the Hot-Spring Deposit at Cherry Hill, Californiaimary fluid inclusions containing oil occur in Stages I–II and VII–XI of 12 paragenetic stages. Stages during which gold was deposited in some cases trapped bitumen and/or oil (IX) and in other cases did not (V and VI). Homogenization temperatures (T.) of primary oil inclusions in general de-crease
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