paralic

paralic

[pə′ral·ik]
(geology)
Pertaining to deposits laid down on the landward side of a coast.
References in periodicals archive ?
The high ash seems to be due to presence of these coal near margin of swamps and probably the paralic nature of these swamps give rise to high sulphur, according to calorific value the rank of these coal ranges for subbituminous B to medium volatile bituminous, highest rank in Pakistan coals.
In the early Middle Jurassic (Aalenian - Bajocian), ephemeral coastal to paralic, brackish to freshwater, environments developed: they consists of well-bedded marly to clayey deposits rich in charophytes, lacustrine ostracods and microflora (Ashraf et al.
2013) Stratum Upper series Shiqianfeng Formation Permian Middle series Shihezi Formation Upper Lower series Shanxi Paleozoic Formation Upper series Taiyuan Formation Carboniferous Middle Benxi series Formation Main Thickness (m) main lithology sedimentary facies mud shale, 100-250 paralic lakes sandstone the upper is pelite intercalating sandstone; 120-570 lakes, rivers lower is interbedded sandstone and shale coal seam, 100-400 delta and sandstone, tidal flat mud shale coal seam, sandstone, mud shale, 50-400 tidal flat and carbonatite coal seam, interbedded sandstone and 0-560 lagoon and shale, tidal flat intercalating carbonatite Table 3.
shallow marine paralic (at or near sea level) and shelf sands laid down on an unconformable surface of a regressive marine shale (Barnes and others, 1996); and
Mining activities are conducted there in the layers of the Mudstone Series and Paralic Series (marginal upper beds).
Paralic (2009) Distributed task-based execution engine for support of text-mining processes, Proceedings of the 7th International Symposium on Applied Machine Intelligence and Informatics, SAMI 2009, pp.
The Lucaogou Formation was formed in a large-scale paralic lacustrine basin with very high organic matter productivity in a reducing water environment favorable to preservation of organic matter.
Distribution of diagenetic alterations in fluvial and paralic deposits within sequence stratigraphic framework: evidence from the Petrohan Terrigenous Group and the Svidol Formation, Lower Triassic, NW Bulgaria.
Plesiosaur remains from non-marine to paralic sediments.
We can date the resultant lagoon-barrier coasts and their relative ages of formation based on limited radiocarbon age determinations in the paralic sedimentary sequences.
1:45 PARALIC SANDS OF THE COAL BLUFF MEMBER OF THE NAHEOLA FORMATION IN MISSISSIPPI, AN OUTCROP OF THE ANCIENT SHORELINE