orogenic in English

adjective

of the formation of mountains; of orogeny

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Below are sample sentences containing the word "orogenic" from the English Dictionary. We can refer to these sentence patterns for sentences in case of finding sample sentences with the word "orogenic", or refer to the context using the word "orogenic" in the English Dictionary.

1. The andesites exhibit “orogenic” chemical features.

2. Isochemical alterations of rock and ore minerals were produced during intensive orogenic processes.

3. These minerals were formed in subduction or obduction zones of alpine-type (high-pressure) orogenic belts.

4. This orogenic pulse (Shawinigan) is not accretionary, but represents a strongly partitioned, compressive, intraplate reactivation event.

5. Orogenic gold mineralization is associated with quartz veins that are surrounded by hypozonal potassic and sulfidic alteration zones.

6. The mainly orebody is typic arrangement assemblage feature of sulphide of sediment orogenic copper ore because primary mineral has obviously zonation.

7. The effects of two phases of deformation in Cretaceous rocks of the Alpine Orogenic Zone of south-eastern Turkey are described.

8. The Altaid orogenic collage hosts numerous gold, silver, copper–molybdenum, lead–zinc, and nickel deposits of Late Proterozoic to Early Mesozoic age

9. Amphibolites are hornblende-plagioclase rocks of metamorphic origin that are widely distributed, especially in Precambrian shield areas and in younger orogenic belts

10. The North China Craton (NCC) was originally formed by the amalgamation of the eastern and western blocks along an orogenic belt at ∼1.9 Ga

11. 22 The development and evolution of Qinling-Dabie orogenic belt is quite similar to the formation and splitting of the Pangea since Phanerozoic eon.

12. 10 The main A-type subduction fault and large scale thin-skinned tectonics clearly reveal that the Yangtze Plate subsides towards Dabie orogenic belt.

13. At a larger scale, the seismic data identify a variety of orogenic styles ranging from thin- to thick-skinned accretion in the Cordillera and crustal-scale tectonic wedging associated with both Paleoproterozoic and Mesozoic collisions.

14. The occurrence ofMiyashiro's andalusite-sillimanite type and low-pressure intermediate group of regional metamorphism in orogenic belts of widely different age merely signifies that in all these belts granitic magma that was formed in depth, rose to higher levels.

15. The Junggar, Turfan and Alakol basins in northwestern China and Kazakhstan formed as Late Permian to ?Early Triassic extensional structures in a broad sinistral shear zone between large strike-slip faults that separate two main domains of the Altaid orogenic collage

16. This Au ore upgrading model, referred to as “Aseismic refinement,” provides a new insight for the genesis of ultrarich Au mineralization and, based on textures reported from many Au deposits, may be a globally significant component in the formation of orogenic Au deposits.

17. Moreover, according toMiyashiro regional metamorphism of his kyanite-sillimanite type (= Dalradian or Barrovian type) was common in Palaeozoic time, whereas that of his andalusite-sillimanite type and low-pressure intermediate group (Buchan type) took place in orogenic belts of Precambrian as well as Palaeozoic and Mesozoic age.

18. Lepidolite and lithian muscovite occur in high-pressure spodumene, low-pressure petalite, phosphorus-enriched amblygonite and fluorine-rich lepidolite subtypes of orogenic affiliated complex type granitic pegmatites and rarely in anorogenic affiliated amazonite-bearing Trace element data determined by X-ray fluorescence for lepidolite of various pegmatite subtypes, morphology (“book”, “scaly”, “fine-grained”), position within the pegmatite (primary zones, replacement units, pockets), mineral assemblages and tectonic affinity (orogenic vs anorogenic) show extreme fractionation of Rb and Cs; modest levels of T1, Ga, Nb, Ta, Sn and Zn; and typically low abundances of Ba, Sr, Ni, Pb, Y, V, W and Zr.

19. Caledonian orogenic belt, range of mountains situated in northwestern Europe, developed as a result of the opening, closure, and destruction of the Iapetus Ocean in the period from the start of the Cambrian (542 million years ago) to the end of the Silurian (about 416 million years ago).