Research Article

Multiple Influences of Paleogeography, Sequence Stratigraphy, and Fold Structure on Coalbed Methane Accumulation in the Lopingian (Late Permian) of Junlian Coalfield, SW China

Table 1

Dominant lithofacies of the Lopingian coal-bearing strata in southern Sichuan.

Lithological typesLithofaciesLithologyEnvironmental interpretation

Conglomerate(1) ConglomerateFine- to medium-grained conglomerate, low maturity, thin-beddedChannel lag deposit
Sandstone(2) Massive bedded sandstoneGrayish white and gray, thick-bedded, well-sorted, angular-subangular, with basal erosional surface and plant fossilsFluvial channel deposit, delta plain distributary channel, and mouth bar
(3) Tabular cross-bedded sandstoneGrayish white and gray, thick-bedded, well-sorted and well-rounded, basal erosional surfaceMouth bar, point bar deposit, and distributary channel
(4) Wedge cross-bedded sandstoneGray and brownish gray, thick-bedded, with mudstone gravels and plant fossils, basal erosional surfaceDelta plain distributary channel and mouth bar
(5) Trough cross-bedded sandstoneGray white, thick-bedded, few gravels, with basal erosional surface, common mud at the bottomPoint bar of fluvial channel, distributary channel, and mouth bar
(6) Parallel-bedded sandstoneFine to medium-grained sandstone, gray white, medium and thick-bedded, with parting lineationDistributary channel and tidal flat deposit
(7) Wavy cross-bedded sandstoneGrayish white and gray, thick-bedded, with animal and plant fossils, abundant trace fossilsDistributary channel, tidal flat, and flood plain
(8) Two-way cross bedded sandstoneGrayish white and gray, thick-bedded, with animal and plant fossils, abundant trace fossilsDistributary channel, tidal channel
Siltstone(9) Horizontally bedded siltstoneGrayish brown-grayish black, thin-bedded, animal and plant fossils with argillaceous inclusion locallyFlood basin, interdistributary bays, delta front, and lagoon
(10) Wavy cross-bedded siltstoneLight gray siltstone and dark gray mudstone interbedded, visible storm disturbance, and biological disturbance structureOverbank and tidal flat
Mudstone(11) Carbonaceous mudstoneGrayish black and black, often pyritePeat swamp
(12) Massive mudstonePurple and gray black, medium and thick-bedded, with animal and plant fossils, often pyrite and siderite, and occasionally biological fossilsLagoon, interdistributary bays
(13) Horizontally bedded mudstoneGray and gray black, medium and thick-bedded, with animal and plant fossilsDelta plain interdistributary bays, lagoon
(14) Bauxitic mudstoneGrayish white, thick-beddedLagoon
(15) Root claystoneGray and white, rich in root fossilsPeat swamp and lagoon
(16) Sideritic mudstoneGray and gray black, thick bedding, with high proportionLagoon
(17) Volcanic ash altered claystoneWhite-light gray, sticky when exposed to water, often as coal seam ganguePeat swamp and backswamp
Limestone(18) Bioclastic limestoneGray, thick-bedded, abundant fossil bioclastsCarbonate platform
(19) Muddy limestoneLight gray-dark gray, thick-beddedCarbonate platform
Coal(20) CoalBlack, thin-medium and thick-bedded, coal composition is dominated by vitrinite, cleat developmentPeat swamp