Optical Evolution of Exinite Euring Coalification Based on the Discovery of the Anisotropical Exinite
-
摘要: 通过对我国几个典型煤田300多块煤光片的详细煤岩研究,发现煤中存在一种高反射具强烈各向异性的有机显微组分,有些保存了完好的壳质组外形和结构.可称之为各向异性壳质组,它广泛分布于长焰煤以上各煤级煤中,它的发现进一步说明了壳质组的煤化历程是复杂的。有些在煤化过程中几乎全部裂解为烃类而消失,绝大多数光性与共生镜质组同化,还有一少部分转变成了各向异性壳质组。Abstract: Having studied the detailed coal petrological characteristics of more than 300 polished coal blocks sampled from eleven coalfields in China the authors have discovered a kind of organic maceral in coals with a high reflectance and strong anisotropy. Some of it conserves clearly the appearance and structure of exinite.According to the original maceral which is changed into anisotropic exinite. it can be divided into six types: anisotropic alginite. anisotropic sporinite. anisotropic cutinite. anisotropic exsudatmite. anisotropic bituminite and anixotropic liptodetrinitc. furthermore there is an amorphous anisotropic matter in coals. Anisotropic exinite is formed gradually by some of exinite during the coalifieation.ft occurs first in flame coal stage, and distributes frequently in coals with rank higher than gas coal stage. The statistics show that the content of anisotropic exinite in coals investigated varies from zero to 1.8%. and that the total content of anisotropic matter in coals is less than 12.74%. commonly from 1.0 to 4.0%. which is much less than that of exinite in specimens sampled from the same coal and the similar coal petrological type, but different coal rank. Since the changing of coal- forming environments and the difference of coal- forming plants, the exinite of same type may have different characteristics.The fluorescent intnsity and reflectance of exinite is the mark of its thermal activities, which will control its evolution processes and final products during the coalirlcation.On the bases of these facts, therefore, the exinite can be grouped into three types according to their optical evolution during the coahfication: l.Thc exinite of extreme thermal activity, such as fluorinite. terpenite and so on. evolutes completely into hydrocarbons. 2.The exinite of large thermal activity, such as some of alginite, resinite, sporinite, cutinite and so on, change into the anisotropic exinite as they draining off the liquid hydrocarbon. 3.And the exinite with less thermal activity shares gradually the same optical properties with intergrowth vitrinite during the coalification.
-
[1] 1. 肖贤明、任德贻，1988,《中国矿业学院学报》，第2期，77-83页。
2. J.布鲁克斯主编，高品文译，1987，有机质成熟作用研究与矿物燃料勘探，石油工业出版社，175-187页。
3. Goodarzi F.，1985. Optically anisotropic fragments in a Western Cannadian subbituminous coal. (Fuel)，1985.N0.9.
4. Jones J. M.，et al.，1977, Optical character of thermally metamophosed coals of 'Yorthern England, Journal of Microscopy. 1977. Vo1.109, p.1.
5. Ren Deyi, et al.，Study of the anisotropinite of thermally metamorphosed coals in we,tern Henan. in 11th international congress of Carboniferous stratiography and geology，Abstracts of Papers.p.261-262.
6. Stach E.、et al.，1932. Stach' s textbook coal petrology. 3rd revised and enlarged edition.
Gebruder Borntraeger. Berlin.p.125-127: 348-356.
7. Teichmuller M.，1973, Generation of petroleum-like substances m coal seams as seen under the mi-croscope. In: Advances in Organic Geochemistry. 1973, p.379-408. -
点击查看大图
计量
- 文章访问数: 405
- HTML全文浏览量: 0
- PDF下载量: 403
- 被引次数: 0
下载:
