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The component variation of terrigenous organic matter and the sum of vitrinite, inertinite, sporinite, resinite, cutinite, fluorinite, and alginite (the sum of lamalginite and telalginite, Table 2) are plotted respectively in Figure 2c and Figure 3c-d.
The oil shale samples from [J.sub.2][sh.sup.2] were characterized by the relatively high contents of alginite (average 46 vol%) and biturninite (average 25 vol%) (Fig.
4) and derived from aquatic organisms, including alginite and biturninite (Fig.
Caption: FIGURE 5: Organic constituent (a) and P-A-E ternary diagrams of Wenchang source rocks (b) and Enping source rock (c) (P: higher terrestrial plant; A: amorphous organic matter and alginite; E: exinite and sporonin).
The dark alginite bodies are separated from each other by a matrix of medium gray vitrinite.
Influence of alginite in the reflectance of vitrinite from Joadja, N.S.W., and some other coals and oil shales containing alginite.
The kerogen mainly consists of degraded alginite with a characteristic laminated microtexture (lamalginite), rarely of telalginite.
The low-ash coal seams were mainly formed in the freshwater paleoenvironment in the low-lying mire and the high-ash coal seams were primarily formed in the fluvio-lacustrine environment, the source of organic matter in coal seams being mostly conifers with little alginite supply [20].
Microscopic studies for selected oil shale samples (Table 2) define an organic matter assemblage consisting predominantly of alginite and amorphous material [23] which shows apparently a higher proportion of type I kerogen relative to the inferred proportion from Rock-Eval data and especially [S.sub.2]/[S.sub.3] ratios.
Varieties of sulphur in the alginite sequence of Kossen facies from the borehole Rezi Rzt-1 W-Hungary // Oil Shale.
Reflected light microscopy and micro-FTIR of upper Ordovician Cloeocapsomorpha prisca alginite in relation to paleoenvironment and petroleum generation, Saskatchewan, Canada // Org.
Alginite is the predominant organic matter in kerogen type I.
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