| Plural | metamorphisms |
contact metamorphism
metamorphism na kontak
regional metamorphism
metamorphism na rehiyonal
dynamic metamorphism
metamorphism na dinamiko
Concepts of metamorphism, metamorphic reaction, prograde and retro – metamorphisms.
Konsepto ng metamorphism, reaksiyong metamorphic, prograde at retro – metamorphism.
It has a prismatic and splintery texture and is abundant in regionally metamorphosed (see metamorphism) rocks such as schists.
Ito ay may prismatic at splintery na tekstura at sagana sa mga rehiyonal na metamorphosed (tingnan ang metamorphism) na mga bato tulad ng schists.
Thus, the boron-bearing rock system and the magnesian rocks are the foundation of the borate deposits, whereas regional metamorphism and migmatitization and tectonism are the necessary conditions.
Kaya naman, ang sistemang batong naglalaman ng boron at ang mga batong magnesian ang pundasyon ng mga deposito ng borate, samantalang ang rehiyonal na metamorphism, migmatitization, at tektonismo ang mga kinakailangang kondisyon.
Xiaertai rock group,a set of metamorphic rock system in Xiaertai area,has experienced strong ductilebrittle deformation and then thermal contact metamorphism and dynamometamorphism in the late stage.
Ang Xiaertai rock group, isang set ng sistemang batong metamorphic sa lugar ng Xiaertai, ay nakaranas ng malakas na ductilebrittle deformation at pagkatapos ay thermal contact metamorphism at dynamometamorphism sa huling yugto.
No.39 coal is one of high-metamorphism anthracite with black color and near-metallic luster in which semibright coal and semidull coal are dominant lithetype and there is a little dull coal.
Ang No.39 coal ay isa sa mga high-metamorphism anthracite na may itim na kulay at malapit na metallic na kinang kung saan ang semibright coal at semidull coal ay nangingibabaw na lithetype at may kaunting dull coal.
The former three stages reflect the major process of eclogite facies metamorphism and the latest stages the light overprinting of greenschist facies retrometamorphism at the shallow level of crust.
Ang unang tatlong yugto ay sumasalamin sa pangunahing proseso ng metamorphism ng facies ng eclogite at ang pinakahuling yugto ang magaan na pag-iimprenta ng retrometamorphism ng facies ng greenschist sa mababaw na antas ng crust.
contact metamorphism
metamorphism na kontak
regional metamorphism
metamorphism na rehiyonal
dynamic metamorphism
metamorphism na dinamiko
Concepts of metamorphism, metamorphic reaction, prograde and retro – metamorphisms.
Konsepto ng metamorphism, reaksiyong metamorphic, prograde at retro – metamorphism.
It has a prismatic and splintery texture and is abundant in regionally metamorphosed (see metamorphism) rocks such as schists.
Ito ay may prismatic at splintery na tekstura at sagana sa mga rehiyonal na metamorphosed (tingnan ang metamorphism) na mga bato tulad ng schists.
Thus, the boron-bearing rock system and the magnesian rocks are the foundation of the borate deposits, whereas regional metamorphism and migmatitization and tectonism are the necessary conditions.
Kaya naman, ang sistemang batong naglalaman ng boron at ang mga batong magnesian ang pundasyon ng mga deposito ng borate, samantalang ang rehiyonal na metamorphism, migmatitization, at tektonismo ang mga kinakailangang kondisyon.
Xiaertai rock group,a set of metamorphic rock system in Xiaertai area,has experienced strong ductilebrittle deformation and then thermal contact metamorphism and dynamometamorphism in the late stage.
Ang Xiaertai rock group, isang set ng sistemang batong metamorphic sa lugar ng Xiaertai, ay nakaranas ng malakas na ductilebrittle deformation at pagkatapos ay thermal contact metamorphism at dynamometamorphism sa huling yugto.
No.39 coal is one of high-metamorphism anthracite with black color and near-metallic luster in which semibright coal and semidull coal are dominant lithetype and there is a little dull coal.
Ang No.39 coal ay isa sa mga high-metamorphism anthracite na may itim na kulay at malapit na metallic na kinang kung saan ang semibright coal at semidull coal ay nangingibabaw na lithetype at may kaunting dull coal.
The former three stages reflect the major process of eclogite facies metamorphism and the latest stages the light overprinting of greenschist facies retrometamorphism at the shallow level of crust.
Ang unang tatlong yugto ay sumasalamin sa pangunahing proseso ng metamorphism ng facies ng eclogite at ang pinakahuling yugto ang magaan na pag-iimprenta ng retrometamorphism ng facies ng greenschist sa mababaw na antas ng crust.
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