Access the full text.
Sign up today, get DeepDyve free for 14 days.
Loading next page...
/lp/emerald-publishing/coal-petrology-and-coal-facies-interpretations-of-bark-liptobiolith-CYyDqbHYIr
References (20)
-
Yuzhuang Sun (2003)
Petrologic and geochemical characteristics of “barkinite” from the Dahe mine, Guizhou Province, ChinaInternational Journal of Coal Geology, 56
-
J. Calder, M. Gibling, P. Mukhopadhyay (1991)
Peat formation in a Westphalian B piedmont setting, Cumberland Basin, Nova Scotia; implications for the maceral-based interpretation of rheotrophic and raised paleomiresBulletin De La Societe Geologique De France, 162
-
Yuzhuang Sun, Cunliang Zhao, Ming-yue Lin, Kankun Jin, S. Ding (2010)
Formation Mechanism of Maceral and Mineral Compositions of the “Barkinite” Liptobiolith from the Jinshan Mine, Anhui Province, ChinaActa Geologica Sinica ‐ English Edition, 84
-
R. Philp, L. Mansuy (1997)
Petroleum Geochemistry: Concepts, Applications, and ResultsEnergy & Fuels, 11
-
Chen Qi (1996)
ORIGIN AND PRECURSORS OF LATE PERMIAN LEPING COAL IN SOUTHERN CHINA -
K. Peters, C. Walters, J. Moldowan (2004)
The Biomarker Guide -
H. Haven, J. Leeuw, J. Rullkötter, J. Damsté (1987)
Restricted utility of the pristane/phytane ratio as a palaeoenvironmental indicatorNature, 330
-
Xuguang Sun (2002)
The optical features and hydrocarbon-generating model of barkinite from Late Permian coals in South ChinaInternational Journal of Coal Geology, 51
-
J. Volkman, J. Maxwell (1986)
acyclic isoprenoids as biological markersMethods in geochemistry and geophysics, 24
-
C. Diessel (1982)
An appraisal of coal facies based on maceral characteristicsAustralian Coal Geology, 4
-
M. Teichmüller (1990)
The genesis of coal from the viewpoint of coal petrologyInternational Journal of Coal Geology, 12
-
N. Zhong, M. Smyth (1997)
Striking liptinitic bark remains peculiar to some Late Permian Chinese coalsInternational Journal of Coal Geology, 33
-
Kenneth Peters, J. Moldowan (1992)
The Biomarker Guide: Interpreting Molecular Fossils in Petroleum and Ancient Sediments -
Chunqing Jiang, R. Alexander, R. Kagi, A. Murray (1998)
Polycyclic aromatic hydrocarbons in ancient sediments and their relationships to palaeoclimateOrganic Geochemistry, 29
-
W. Püttmann, H. Villar (1987)
Occurrence and geochemical significance of 1,2,5,6-tetramethylnaphthaleneGeochimica et Cosmochimica Acta, 51
-
Q. Chen (1995)
Sedimentary environments of longtan plant group and leping coal in southern China (in Chinese)South China Petroleum Geology, 1
-
C. Hsieh (2009)
ON LOPINITE,A NEW TYPE OF COAL IN CHINABulletin of The Geological Society of China, 12
-
M. Radke (1983)
The Methylphenanthrene Index (MPI) : a maturity parameter based on aromatic hydrocarbons -
G. Ourisson, P. Albrecht, M. Rohmer (1979)
The Hopanoids: palaeochemistry and biochemistry of a group of natural productsPure and Applied Chemistry, 51
-
Q. Chen (1996)
Origin and precursors of late permian leping coal in southern China (in Chinese)Marine Origin Petroleum Geology
- Publisher
- Emerald Publishing
- Copyright
- Copyright © Emerald Group Publishing Limited
- ISSN
- 1708-5284
- DOI
- 10.1260/1708-5284.10.3.253
- Publisher site
- See Article on Publisher Site
Abstract
A detailed analytical study of Leping bark liptobiolith in Jiangxi was conducted to determine its petrographic characteristics and depositional environment based on coal petrography and geochemistry. Results indicate that barkinite mainly occurs in the middle and lower coal sea4ms, whereas less barkinite and more vitrinite occur in the middle and upper coal seams. Coal facies analysis of bark liptobiolith was performed to determine its characteristics under various depositional conditions, such as the presence of a water table and gelification during coal formation. Results indicate that the environmental evolution of bark liptobiolith begins from brackish-marine swamp facies (barkinite-rich coal seam) and ends in back barrier swamp facies (barkinite-poor coal seam).
Journal
World Journal of Engineering – Emerald Publishing
Published: Sep 1, 2013