| Plural | tectonics |
tectonic plate
plakang tektoniko
tectonic activity
aktibidad na tectonic
tectonic boundary
hangganan ng tektoniko
tectonic stress
tectonic stress
tectonic movement
paggalaw ng mga tectonic
tectonic setting
tektonikong setting
tectonic analysis
pagsusuri ng tektoniko
tectonic facies
tektonikong anyo
the violent convulsions of tectonic plates.
ang marahas na pagyanig ng mga tectonic plate.
Argand's mobilism thought as to the dynamical evolution process of the tectonics in On Major Tectonic Forms of China. Then, he absorbed the quintessence of A.
Pinaniniwalaan ni Argand na ang mobilismo ay may kaugnayan sa proseso ng ebolusyon ng dinamika ng mga tectonic sa On Major Tectonic Forms of China. Pagkatapos, inabsorba niya ang esensya ng A.
Dongting basin was shaped not only by tectonic movement but also by potamic and anthropogenic influence.
Ang Dongting basin ay hindi nabuo lamang ng tectonic movement kundi pati na rin ng potamic at impluwensya ng tao.
This crisis possibly causes the world civilized tectonic plate's constructivity migration.
Ang krisis na ito ay posibleng magdulot ng paglipat ng konstruksyon ng tectonic plate sa buong mundo.
The sequence classification and dynamic analysis of this basin provide an important evidence to the stratigraphic correlation, tectonic analysis and minerogenesis.
Ang pag-uuri ng pagkakasunud-sunod at ang dynamic na pagsusuri ng basin na ito ay nagbibigay ng mahalagang ebidensya sa stratigraphic correlation, tectonic analysis, at minerogenesis.
As is well known the regional tectonic stress field is of great importance to the study of seismogenesis, earthquake prediction and earth dynamics.
Tulad ng kilala, ang rehiyonal na larangan ng stress na tectonic ay napakahalaga sa pag-aaral ng seismogenesis, paghula ng lindol, at dinamika ng Earth.
Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.
Pagkatapos, gamitin ang antitone structural analysis method upang kilalanin at muling buuin ang pangunahing tectonic structure at sedimentary feature ng isang basin sa ilang geological history.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
Ang tectonic stress field sa mga lugar ng bulkan ng Tengchong ay nakahanay bilang NNE-NE-NEE, papalapit sa pahalang na compressive stress field.
1. the backbone fault of the nappe tectonic was not “F.2”, but within the anhydrite member underlaid the nappe, and the anhydrock was an ideal lubricating layer;
1. Ang backbone fault ng nappe tectonic ay hindi “F.2”, ngunit sa loob ng anhydrite member na nakapatong sa ilalim ng nappe, at ang anhydrock ay isang ideal na lubricating layer;
The styles of the detachment structure are short antiform and synform structure mainly, and dome structure, nappe outlier and nappe tectonic window too.
Ang mga estilo ng istraktura ng detachment ay pangunahin ang maikling antiform at synform structure, at dome structure, nappe outlier at nappe tectonic window din.
The atectonic movement is the dominant factor for developing the slope breaks,and the scale of slope breaks intimately relates with the size of tectonic movement.
Ang paggalaw ng tectonic ay ang pangunahing salik sa pagbuo ng mga pagkasira ng dalisdis, at ang sukat ng mga pagkasira ng dalisdis ay malapit na nauugnay sa laki ng paggalaw ng tectonic.
Suo Shutian.Zhong Zengqiu.You Zhendong Extensional tectonic framework of the Dabie-Sulu UHP-HP metamorphic belt,central China,and its geodynamical significance 2001(1
Suo Shutian.Zhong Zengqiu.You Zhendong Extensional tectonic framework ng Dabie-Sulu UHP-HP metamorphic belt, sentral na Tsina, at ang geodynamical significance nito 2001(1
ynamic metamorphous features and evolutionary process of tectonic coal have been studied by X-ray diffraction and electron spin resonance(ESR).
Ang dynamic metamorphous features at evolutionary process ng tectonic coal ay pinag-aralan sa pamamagitan ng X-ray diffraction at electron spin resonance(ESR).
, suggesting the significant shifting of sediment provenance, the stable trending of tectonic movement, and the wet and torridity aridity of paleoclimate condition.
Nagpapahiwatig ng malaking pagbabago sa pinagmulan ng sediment, ang matatag na pagbabago ng paggalaw ng tektoniko, at ang basa at maalat na aridity ng kondisyon ng paleoclimate.
By using the approach of morphostructure and tectonic chronology analysis, neotectonic activity evidences and characteristics as well as its ralation to uranium mineralization were researched.
Sa pamamagitan ng paggamit ng pamamaraan ng pagsusuri ng morphostructure at tectonic chronology, sinuri ang mga ebidensya at katangian ng neotectonic activity pati na rin ang kaugnayan nito sa uranium mineralization.
Characteristics of plastic deformation of stress minerals in veins, such as subgrain tectonics, deformation, lamellae and deformation bands, can be found.
Ang mga katangian ng plastic deformation ng mga mineral na may stress sa mga ugat, tulad ng subgrain tectonics, deformation, lamellae, at deformation bands, ay maaaring matagpuan.
Photo Gallery: Plate Tectonics Sulfur, salt, and other minerals color the crater of Dallol volcano, part of the Danakil Depression in Ethiopia.
Mga Litratong Gallery: Tektonika ng mga Plate Ang asupre, asin, at iba pang mineral ay nagkulay sa crater ng bulkan na Dallol, bahagi ng Danakil Depression sa Ethiopia.
The reasons forming abnormal formation pressure mainly includes digenesis, thermogenesis, biochemical action, tectonic action, dialysis, and fluid density difference action.
Ang mga dahilan na bumubuo sa abnormal na formation pressure ay pangunahin na kinabibilangan ng digenesis, thermogenesis, biochemical action, tectonic action, dialysis, at fluid density difference action.
The protocontinent of the Southern Hemisphere, a hypothetical landmass that according to the theory of plate tectonics broke up into India, Australia, Antarctica, Africa, and South America.
Ang protocontinent ng Southern Hemisphere, isang hypothetical landmass na ayon sa teorya ng plate tectonics ay naputol sa India, Australia, Antarctica, Africa, at South America.
The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.
Ang modelo ng tectonic ng palanggana: ito ay intermont basin noong huling Jurassic hanggang unang Cretaceous, napaunlad sa faulted-lacustrine basin sa Eogene, at naging depression sa Neogene at Quaternary.
tectonic plate
plakang tektoniko
tectonic activity
aktibidad na tectonic
tectonic boundary
hangganan ng tektoniko
tectonic stress
tectonic stress
tectonic movement
paggalaw ng mga tectonic
tectonic setting
tektonikong setting
tectonic analysis
pagsusuri ng tektoniko
tectonic facies
tektonikong anyo
the violent convulsions of tectonic plates.
ang marahas na pagyanig ng mga tectonic plate.
Argand's mobilism thought as to the dynamical evolution process of the tectonics in On Major Tectonic Forms of China. Then, he absorbed the quintessence of A.
Pinaniniwalaan ni Argand na ang mobilismo ay may kaugnayan sa proseso ng ebolusyon ng dinamika ng mga tectonic sa On Major Tectonic Forms of China. Pagkatapos, inabsorba niya ang esensya ng A.
Dongting basin was shaped not only by tectonic movement but also by potamic and anthropogenic influence.
Ang Dongting basin ay hindi nabuo lamang ng tectonic movement kundi pati na rin ng potamic at impluwensya ng tao.
This crisis possibly causes the world civilized tectonic plate's constructivity migration.
Ang krisis na ito ay posibleng magdulot ng paglipat ng konstruksyon ng tectonic plate sa buong mundo.
The sequence classification and dynamic analysis of this basin provide an important evidence to the stratigraphic correlation, tectonic analysis and minerogenesis.
Ang pag-uuri ng pagkakasunud-sunod at ang dynamic na pagsusuri ng basin na ito ay nagbibigay ng mahalagang ebidensya sa stratigraphic correlation, tectonic analysis, at minerogenesis.
As is well known the regional tectonic stress field is of great importance to the study of seismogenesis, earthquake prediction and earth dynamics.
Tulad ng kilala, ang rehiyonal na larangan ng stress na tectonic ay napakahalaga sa pag-aaral ng seismogenesis, paghula ng lindol, at dinamika ng Earth.
Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.
Pagkatapos, gamitin ang antitone structural analysis method upang kilalanin at muling buuin ang pangunahing tectonic structure at sedimentary feature ng isang basin sa ilang geological history.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
Ang tectonic stress field sa mga lugar ng bulkan ng Tengchong ay nakahanay bilang NNE-NE-NEE, papalapit sa pahalang na compressive stress field.
1. the backbone fault of the nappe tectonic was not “F.2”, but within the anhydrite member underlaid the nappe, and the anhydrock was an ideal lubricating layer;
1. Ang backbone fault ng nappe tectonic ay hindi “F.2”, ngunit sa loob ng anhydrite member na nakapatong sa ilalim ng nappe, at ang anhydrock ay isang ideal na lubricating layer;
The styles of the detachment structure are short antiform and synform structure mainly, and dome structure, nappe outlier and nappe tectonic window too.
Ang mga estilo ng istraktura ng detachment ay pangunahin ang maikling antiform at synform structure, at dome structure, nappe outlier at nappe tectonic window din.
The atectonic movement is the dominant factor for developing the slope breaks,and the scale of slope breaks intimately relates with the size of tectonic movement.
Ang paggalaw ng tectonic ay ang pangunahing salik sa pagbuo ng mga pagkasira ng dalisdis, at ang sukat ng mga pagkasira ng dalisdis ay malapit na nauugnay sa laki ng paggalaw ng tectonic.
Suo Shutian.Zhong Zengqiu.You Zhendong Extensional tectonic framework of the Dabie-Sulu UHP-HP metamorphic belt,central China,and its geodynamical significance 2001(1
Suo Shutian.Zhong Zengqiu.You Zhendong Extensional tectonic framework ng Dabie-Sulu UHP-HP metamorphic belt, sentral na Tsina, at ang geodynamical significance nito 2001(1
ynamic metamorphous features and evolutionary process of tectonic coal have been studied by X-ray diffraction and electron spin resonance(ESR).
Ang dynamic metamorphous features at evolutionary process ng tectonic coal ay pinag-aralan sa pamamagitan ng X-ray diffraction at electron spin resonance(ESR).
, suggesting the significant shifting of sediment provenance, the stable trending of tectonic movement, and the wet and torridity aridity of paleoclimate condition.
Nagpapahiwatig ng malaking pagbabago sa pinagmulan ng sediment, ang matatag na pagbabago ng paggalaw ng tektoniko, at ang basa at maalat na aridity ng kondisyon ng paleoclimate.
By using the approach of morphostructure and tectonic chronology analysis, neotectonic activity evidences and characteristics as well as its ralation to uranium mineralization were researched.
Sa pamamagitan ng paggamit ng pamamaraan ng pagsusuri ng morphostructure at tectonic chronology, sinuri ang mga ebidensya at katangian ng neotectonic activity pati na rin ang kaugnayan nito sa uranium mineralization.
Characteristics of plastic deformation of stress minerals in veins, such as subgrain tectonics, deformation, lamellae and deformation bands, can be found.
Ang mga katangian ng plastic deformation ng mga mineral na may stress sa mga ugat, tulad ng subgrain tectonics, deformation, lamellae, at deformation bands, ay maaaring matagpuan.
Photo Gallery: Plate Tectonics Sulfur, salt, and other minerals color the crater of Dallol volcano, part of the Danakil Depression in Ethiopia.
Mga Litratong Gallery: Tektonika ng mga Plate Ang asupre, asin, at iba pang mineral ay nagkulay sa crater ng bulkan na Dallol, bahagi ng Danakil Depression sa Ethiopia.
The reasons forming abnormal formation pressure mainly includes digenesis, thermogenesis, biochemical action, tectonic action, dialysis, and fluid density difference action.
Ang mga dahilan na bumubuo sa abnormal na formation pressure ay pangunahin na kinabibilangan ng digenesis, thermogenesis, biochemical action, tectonic action, dialysis, at fluid density difference action.
The protocontinent of the Southern Hemisphere, a hypothetical landmass that according to the theory of plate tectonics broke up into India, Australia, Antarctica, Africa, and South America.
Ang protocontinent ng Southern Hemisphere, isang hypothetical landmass na ayon sa teorya ng plate tectonics ay naputol sa India, Australia, Antarctica, Africa, at South America.
The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.
Ang modelo ng tectonic ng palanggana: ito ay intermont basin noong huling Jurassic hanggang unang Cretaceous, napaunlad sa faulted-lacustrine basin sa Eogene, at naging depression sa Neogene at Quaternary.
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