granitic in English
adjective
[gra·nit·ic || græ'nɪtɪk]
like granite; of or pertaining to granite
Use "granitic" in a sentence
1. A granitic rock composed chiefly of quartz and mica.
2. The Batholith is characterized by granitic soils and
3. Fractionation of hornblende, biotite and andesine yields granitic magmas.
4. Granitic gneiss is composed of quartz, plagioclase, Biotite, and microcline
5. The Abbor-Alz hills are rocky, granitic, and generally have
6. The entire area lies thermally above the melting of rocks of granitic composition.
7. Geochemical analyses experimentally corroborate the data generally accepted about granitic rocks alterability.
8. A batholith has been defined as a huge intrusive mass of granitic rock.
9. ‘Metamorphic Aureoles around the granitic rocks are estimated to extend on the order of 1 km from the granitic rocks.’ More example sentences ‘This is the widest metamorphic zone in the aureole.’
10. One major difference between Basaltic and granitic magma is their specific mineral contents
11. The Columbite in the Zhaojinggou deposit crystallized from a highly evolved peraluminous granitic magma
12. Tai Shan is granitic while Lao Shan has soluble limestone with mineral water springs.
13. Conglomerates, arkoses, and acidic volcanics may all metamorphose to foliated rocks of granitic composition.
14. Azorite: A mineral crystallizing in tetragonal crystals, found in a granitic rock in the Azores
15. The interior of the main continental landmass includes an extensive granitic core called a craton.
16. The Idaho Batholith is a composite mass of granitic plutons covering approximately 15,400 square miles in central Idaho
17. Contact metamorphism of the hornblende hornfels and albite–epidote hornfels facies has been induced by the granitic intrusions.
18. They intersect Precambrian country rocks composed of potassium feldspar-biotite-granitic-mobilisates and chloritised biotite mica schists.
19. Beryl is a minor constituent of many granitic rocks and associated pegmatite dikes, in gneisses, and in mica schists
20. This conical granitic rock, rising about 1,300 feet (395 m), stands like a sentinel at the entrance to Guanabara Bay.
21. The contrast between gas-rich and gas-poor magmas is much more pronounced at the viscous granitic end of the scale.
22. Batholiths are composite masses of granitic rocks having areas ranging from tens of square miles to tens of thousands of square miles
23. Arkose is a sand or sandstone with considerable feldspar content, derived from weathering and erosion of a (usually nearby) granitic rock outcrop.
24. Hydrothermal fluids released by the cooling granitic magmas then transported those isotopes along the Biotites’ cleavage planes to deposit the Po isotopes in
25. The Borid series consists of shallow, somewhat excessively drained soils with moderately rapid permeability that formed in colluvium and residuum from granitic rocks
26. Extreme variation and apparent reversal of Nb-Ta fractionation in Columbite-group minerals from the Scheibengraben beryl-Columbite granitic pegmatite, Marsikov, Czech Republic
27. Batholiths usually are granitic (see granite) in composition, have steeply inclined walls, have no visible floors, and commonly extend over areas of thousands of …
28. Batholiths usually are granitic (see granite ) in composition, have steeply inclined walls, have no visible floors, and commonly extend over areas of thousands of …
29. Most granitic Batholiths contain plutons which are composed of low-variance mineral assemblages amenable to quantification of the P – conditions that characterise emplacement
30. Contamination and assimilation of andesitic and »shoshonitic« rocks by uprising granitic magmas generated, in association with hydrothermal phenomena, composite environments for gold deposits.
31. Within the belt , the mid-late Proterozoic (epimetamorphic) green- schists were ovethrust from south to north onto the late Paleozoic granitic batholith at a low angle.
32. Development of a more basic rock, usually with more hornblende, biotite, and oligoclase, by contamination of a granitic magma in the assimilation of country Explanation of Basify
33. A double Soxhlet extractor was used in the laboratory to perform accelerated chemical weathering tests in order to simulate the leaching of granitic rocks under tropical climate.
34. The fracture of a shear fault containing several unbroken Asperities in a granitic porphyry is examined in detail via acoustic emission (AE) data collected by a high-speed multi-channel waveform recording system
35. The geographical area consists of a crystalline basement formed by the pedogenic development of metamorphic and granitic rocks, including local formations of alterites and formations on colluvial or old residual alluvial soils.
36. The late granite dike suite, comprising late-stage, muscovite- and biotite-bearing quartz – alkali feldspar pegmatite and finer grained granitic lithologies, represents the last magmatic event in the Northern complex emplaced after collision.
37. When refined, Coltan becomes a heat resistant powder, metallic tantalum, which has unique properties for storing electrical charge. Coltan occurs in granitic pegmatites, pockets where the deep seated molten rock crystallized last.
38. A model is presented for the Santa Angélica intrusion: A mantle derived basic magma, probably a fractionated alkali or transitional basalt, intruded the lower crust and induced anatectic melting and production of granitic melts.
39. Basaltic magma contains between 45 and 55 percent silicon dioxide and is high in magnesium, iron and calcium, while granitic magma contains between 65 and 75 percent silicon dioxide and only small amounts of those minerals.
40. A third and the most voluminous granitic unit, the Shoal Bay granite, is an alkali-feldspar-phyric, medium-grained, equigranular biotite–hastingsite granite with hastingsite and annitic biotite interstitial to euhedral plagioclase, anhedral quartz, and perthite crystals.
41. The oldest cleavage (previously published, whole-rock, 40Ar/39Ar plateau ages of 415–395 Ma) dates the onset of crustal thickening, which was followed by voluminous, but short-lived, Late Devonian granitic and minor mafic magmatism (380–370 Ma).
42. The Mount Nansen ore deposit consists of a system of narrow steeply dipping veins in metamorphic rocks of Precambrian to Paleozoic age, andesitic volcanics and granodioritic to granitic intrusives of Mesozoic age, and Cretaceous to early Tertiary dacitic porphyries.
43. 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.
44. Major and trace element chemistry shows that the older series of granitic rocks were formed by differentiation of a calc-alkali magma in situ. The younger dikes are all highly silicic, show limited major element variation, and have been affected by hydrothermal metasomatism.
45. Other articles where Coast Range Batholith is discussed: Alaskan mountains: Physiography of the southern ranges: …massive granitic rocks of the Coast Range Batholith, successively intruded in various stages during the orogeny of the late Mesozoic to early Cenozoic (about 100 to 50 million years ago)
46. Chalcopyrite ore occurs in a variety of ore types, from huge masses as at Timmins, Ontario, to irregular veins and disseminations associated with granitic to dioritic intrusives as in the porphyry copper deposits of Broken Hill, the American cordillera and the Andes.
47. Dal*—diorite and Andesinite: dark gray 2-pyroxene diorite and hornblende metadiorite-light gray Andesinite dall—Bluish green with purple tint (RS) dalz—Dark yellowish green (RS) gs* Granitic rocks, zoisite-biotite-quartz diorite, granodiorite, and quartz mon- zonite gs1—Medium olive green with bluish tint gs2—Olive green (RS)
48. A description is given of scandium-rich ixiolite, (Ta,Nb,Sc,Sn,Fe,Mn,Ti)2O4 in association with pyrochlore, (Ca,Sc,Y,Sn,U)2(Ta,Nb,Ti)2O6(O,OH,F) and bazzite, Be3Sc2Si6O18 from a cleavelandite-amazonite pegmatite occurring as a part of a larger network of granitic pegmatite veins.
49. Two other Calderas are also postulated.-after Authors AB - Precambrian igneous rocks in the St Francois Mountains of SE Missouri consist of silicic volcanic rocks, mostly ash flow tuff, which crop out mostly in the W and SW part of the region, and epizonal granitic plutons which are mostly exposed in …
50. During latest Precambrian time, in northwest Mexico, an about 2,000 m thick sequence of conglomerate, sandy shale and dolomite, containingCollenia, Cryptozoa and other organisms, accumulated on top of the eroded older Precambrian metamorphics and granitic rocks, that formed the northeast flank of the miogeosynclinal part of the ancestral North American Cordilleran Geosyncline, representing a near-shore facies.