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![Phaneritic](https://www.geoforward.com/wp-content/uploads/Cloud-Photos-by-Azad-Kaligi-co-Geo-Foward-768x440.jpeg)
Phaneritic
Phaneritic Definition In geology, the term Phaneritic applies to the texture of an igneous rock. A phaneritic plutonic rock has grains that are large enough to be seen with the naked eye. In fact, this indicates there was a slower rate of magmatic cooling.
![Mafic](https://www.geoforward.com/wp-content/uploads/Cloud-Photos-by-Azad-Kaligi-co-Geo-Foward-768x440.jpeg)
Mafic
Mafic Definition In geology, “mafic” is a term that describes an igneous rock that has an abundance of darker color minerals.
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Connate Water
Connate Water Definition Connate Water: In geology, connate water is groundwater that has been trapped within the pore space of a sedimentary rock since its original deposition. Connate water is also referred to as “fossil water” due to a long history of non-exposure.
![Hydrogen Sulfide Soil Gas](https://www.geoforward.com/wp-content/uploads/Cloud-Photos-by-Azad-Kaligi-co-Geo-Foward-768x440.jpeg)
Hydrogen Sulfide Soil Gas
Hydrogen Sulfide Soil Gas (In Natural Gas) Hydrogen Sulfide: Hydrogen sulfide (H2S) soil gas geologically occurs upon the thermal and microbial decomposition of subsurface organic material deposits. It is typically identifiable in biogenic and petrogenic natural gas sources, along with higher concentrations of methane soil gas. Additionally, nitrogen, oxygen, hydrogen, ethane, and isobutane exist within natural…
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Cation
Cation Cation: In the fields of chemistry and geochemistry, a cation is a positively charged ion. The oppositely charged ion is an anion.
![Feldspars](https://www.geoforward.com/wp-content/uploads/Cloud-Photos-by-Azad-Kaligi-co-Geo-Foward-768x440.jpeg)
Feldspars
Feldspars Feldspars: In the field of geology, and the branch of mineralogy, feldspars are a mineral group, that is the most common amongst the earth’s crust. In fact, there are two types of feldspars: plagioclase feldspar and orthoclase feldspar.