There are several methods to known the source rock maturation.
In petroleum industry commonly used vitrinite reflectance, spore colour index, and Tmax methods. Loptin 1971, proposed one model called TTI modelling. In his model time and temperature both are taken into consideration to calculate the maturation of a source rock. Any chemical reaction, double when increase the 10 deg centigrate, Lopatin assume the rate of maturation is also follow the same double role. An average 100 deg centigrate is sufficient for generate the hyderocarbons so that he has taken 100-110 deg centigrate temperature interval is base interval for his calculation. He assinged n=0 for this iterval. nth temperature interval, the temperature interval will 2n The modelling is begin with construction of burial history curves.
Source rock maturation can be determined by thermal maturation and hydrocarbon generation. There is also an abstract approach which is usually a mixture of different methods.
One of the main methods of identifying rocks is by their method of formation. Igneous rock from melt; metamorphic rock from heat/pressure;sedimentary rock from lithification of sediment or precipitation. Then add in the myriad of possible combinations and percentages of minerals that may comprise the rock, and sometimes the identification of a rock can be a daunting task. Minerals are identified by their chemical composition, their crystalline structure, their specific gravity, hardness, streak, and other physical properties.
'Clemina' granite may be a trade name associated with a decorative rock. Without a sample, identification would not be possible.
The parent rock (protolith) is the rock type that existed before a rock is altered into metamorphic rock. For instance, shale (sedimentary rock) is the parent rock of slate (metamorphic rock).
it depends on the color of the rock
It is called contact metamorphism. It takes place when the magma at high temperature tries to break out from the magma chamber, it then comes into contact with the country rock at high pressure and temperature.
why is the rock identification important
penis rock
both source rocks and reservoir rocks are highly porous. however, the permeabilty of a reservoir rock distinguishes it from a source rock.
Baishou rock is a metamorphic rock. This particular type of rock tends to transform when it is put under any source of heat or source of pressure.
It aids in the identification process, based on chemistry.
It aids in the identification process, based on chemistry.
It is called the streak, an aid to mineral identification.
Hydrocarbonous rock
There are three methods of intrusive igneous rock formation. Igneous rock can form at mid ocean ridges, subduction zones, and at the continental crust if it is pushed together.
There are two methods used to determine the age of a rock or fossil. The first is carbon dating and the second is radiometric dating.
Morocco is a major source of rock phosphate, but not the sole source.
One of the main methods of identifying rocks is by their method of formation. Igneous rock from melt; metamorphic rock from heat/pressure;sedimentary rock from lithification of sediment or precipitation. Then add in the myriad of possible combinations and percentages of minerals that may comprise the rock, and sometimes the identification of a rock can be a daunting task. Minerals are identified by their chemical composition, their crystalline structure, their specific gravity, hardness, streak, and other physical properties.