kerogen वाक्य
उदाहरण वाक्य
मोबाइल
- Macerals found in kerogen source rocks are often observed under the microscope to determine the kerogen maturity of the sedimentary formations.
- Macerals found in kerogen source rocks are often observed under the microscope to determine the kerogen maturity of the sedimentary formations.
- This polymerization usually happens alongside the formation of a mineral component ( geopolymer ) resulting in a sedimentary rock like kerogen shale.
- Type III kerogen involving rocks are found to be the least productive upon pyrolysis and probably the least favorable deposits for oil generation
- Below this zone, heated gas caused retorting process converting kerogen in oil shale to oil shale gas and shale oil vapors.
- The Cenozoic deposits have gas-prone Type III and II kerogen, with up to 2.5 % TOC locally.
- The kerogen that is found in association with the gold deposits almost certainly represents what remains of these Archean photosynthesizing micro-organisms.
- The kerogen in oil shale can be converted to shale oil through the chemical processes of pyrolysis, hydrogenation, or thermal dissolution.
- Different types of kerogen reflecting different initial conditions mature ( i . e . volatilize ) at different temperatures and pressures.
- Anhydrous incubation experiments have shown that the products are generally more depleted in D than their precursors, causing enrichment in residual kerogen.
- Oil shale and similar materials are sedimentary rocks containing kerogen, a complex mixture of high-molecular weight organic compounds, which yield pyrolyzed ).
- The generation of petroleum from the Lower Cruse formation is said to be of type II kerogen that is characterized by high oil to gas ratios.
- Coals are from type III kerogen mostly derived from terrestrial plants, which should have a primary D / H signal sensitive to local meteoric water.
- While still under debate, it appears likely that incorporation of water hydrogen isotopes is the more dominant process for kerogen D-enrichment during catagenesis.
- The kerogen, or bitumen, that is found in association with the gold deposits almost certainly represents what remains of these Archean photosynthesizing micro-organisms.
- The kerogen content of oil shale formations differs widely, and the economic feasibility of its extraction is highly dependent on international and local costs of oil.
- As the organic rich clay is buried under millions of years of sediment accumulation, the clay turns into shale and the organic material transforms into kerogen.
- Although Tmax is not very reliable for high maturity kerogens due to poor pyrolysis peak yields and peak shape, the extent of kerogen transformation can be utilized.
- Technically speaking, oil shales are not always shales and do not contain oil, but are fined-grain sedimentary rocks containing an insoluble organic solid called kerogen.
- There are varying classifications of oil shales depending on their mineral content, type of kerogen, age, depositional history, and organisms from which they are derived.
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