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In the Dunham classification (Dunham, 1962 [11]) system of limestones, a mudstone is defined as a mud-supported carbonate rock that contains less than 10% grains. Most recently, this definition has been clarified as a matrix-supported carbonate-dominated rock composed of more than 90% carbonate mud (<63 μm) component .
The term is based on the word "whet", which means to sharpen a blade, [3] [4] not on the word "wet". The verb nowadays to describe the process of using a sharpening stone for a knife is simply to sharpen, but the older term to whet is still sometimes used, though so rare in this sense that it is no longer mentioned in, for example, the Oxford Living Dictionaries.
A mudstone is a siliciclastic sedimentary rock that contains a mixture of silt- and clay-sized particles (at least 1/3 of each). [5] The terminology of "mudstone" is not to be confused with the Dunham classification scheme for limestones. In Dunham's classification, a mudstone is any limestone containing less than ten percent carbonate grains.
Masayoshi Soken (祖堅 正慶, Soken Masayoshi, born January 10, 1975) is a Japanese video game composer and sound editor who has worked for Square Enix since 1998. Soken is best known for being the lead composer and sound director of Final Fantasy XIV and its expansions and lead composer of Final Fantasy XVI.
A pelite (from Ancient Greek πηλός (pēlós) 'clay, earth') [3] or metapelite is a metamorphosed fine-grained sedimentary rock, i.e. mudstone or siltstone. The term was earlier used by geologists to describe a clay-rich, fine-grained clastic sediment or sedimentary rock, i.e. mud or a mudstone, the metamorphosed version of which would ...
Journeys: Final Fantasy XIV Arrangement Album is an album of arranged songs from the Heavensward and Stormblood expansions, split between piano and rock arrangements and released on June 19, 2019. Several of the eighteen tracks were previously included in The Primals and the Final Fantasy XIV Piano Collections albums. In Tien Hoang of VGMOnline ...
The Whitby Mudstone is a Toarcian (Early Jurassic; Falciferum-Bifrons in regional chronostratigraphy) geological formation in Yorkshire and Worcestershire, England. [1] The formation, part of the Lias Group , is present in the Cleveland and Worcester Basins and the East Midlands Shelf .
The oldest rocks of the ORS sequence (and hence lowest in the sequence), the mudstones of the Raglan Mudstone Formation, are also assigned to the Silurian period, though were once considered to be Devonian. Towards the eastern, southeastern and western margins of the county are successive layers of rocks of Carboniferous age.