arkose वाक्य
उदाहरण वाक्य
मोबाइल
- Built of arkose, a sort of sandstone, the building has an almost perfect harmony supposedly resulting from the application of the ratio of the Golden Number.
- Near its top, the limestone is conglomeratic and pelletoidal, in part, with pebbles and cobbles of limestone, chert, meta-arkose, and quartz.
- Arkose usually contains small amounts of calcite cement, which causes it to'fizz'slightly in dilute hydrochloric acid; sometimes the cement also contains iron oxide.
- The change in topographic expression, color, and the facies change, from quartz arenite, to mudstone and fine-grained arkose & ndash; is gradational.
- The Mutitjulu Arkose is believed to be of about the same age as the dipping to the south west at 85? and have an exposed thickness of at least.
- If there is more plagioclase than there is K-feldspar, the rock is either a plagioclase arkose, a plagioclase subarkose or a lithic plagioclase arkose, respectively.
- If there is more plagioclase than there is K-feldspar, the rock is either a plagioclase arkose, a plagioclase subarkose or a lithic plagioclase arkose, respectively.
- The Pebbly Arkose has been correlated to the Elliot Formation of the Great Karroo Basin, South Africa and the Mpandi Formation of the Thuli Basin in Botswana and Zimbabwe.
- Finally, the Stone Creek ( upper ) member of the Hakatai Shale consists of pale purple or lavender, fine-to coarse-grained, crossbedded coarse arkose.
- The Pebbly Arkose has been correlated to the Angwa Sandstone Formation in the Mana Pools and Cabora Bassa Basins and the Elliot Formation of the Great Karroo Basin, South Africa.
- Kata Tjuta's domes are the eroded remains of sedimentary rock from the seabed, while Uluru is a relict of the coarse grained, mineral-rich sandstone called arkose.
- Although the Dott classification scheme is widely used by sedimentologists, common names like greywacke, arkose, and quartz sandstone are still widely used by non-specialists and in popular literature.
- The arkose sandstone which makes up the formation is composed of grains that show little sorting based on grain size, exhibit very little rounding and the feldspars in the rock are relatively fresh in appearance.
- A third deposit of chrisstanleyite was found in El Chire, La Rioja, Argentina in a cutting calcite vein containing only one selenide-bearing vein through a hematite-rich sandstone and arkose host rocks.
- If there is more K-feldspar than there is plagioclase, or if it is too difficult to make a distinction between the feldspars, the name stays as arkose, subarkose or lithic arkose, respectively.
- If there is more K-feldspar than there is plagioclase, or if it is too difficult to make a distinction between the feldspars, the name stays as arkose, subarkose or lithic arkose, respectively.
- The Arkose Ridge Formation is unmetamorphosed but tilted and slightly folded, and consists of Tertiary ( Late Paleocene to middle Eocene ) sedimentary arkose, shale, sandstone, and conglomerate rocks that are clearly derived from the schists and intrusive rocks to the north.
- The Arkose Ridge Formation is unmetamorphosed but tilted and slightly folded, and consists of Tertiary ( Late Paleocene to middle Eocene ) sedimentary arkose, shale, sandstone, and conglomerate rocks that are clearly derived from the schists and intrusive rocks to the north.
- It comprises the Escarpment Grit formation ( in the Mid-Zambezi and Limpopo basins ) and the Angwa Sandstone Formation ( in the Mana Pools and Cabora Bassa Basins ), overlain by the Pebbly Arkose Formation and the Forest Sandstone Formation, capped by Batoka Formation basalts.
- If the abundances of quartz, feldspars and rock fragments indicate that the rock is an arkose, a subarkose or a lithic arkose, one must then normalize the abundance of feldspars to 100 % and attempt to identify the relative abundances of K-feldspars to plagioclase in the sample.
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