Information om | Engelska ordet GRANODIORITES

Exempel på hur man kan använda GRANODIORITES i en mening

• The predominant species are coarse-grained granodiorites and granites, which are often porphyry and weathered in places.
• The Kulgera Suite is a widespread, voluminous suite of fractionated amphibole-bearing plagioclase rich tonalite to granodiorites of an I-type affinity (Stewart, 2003).
• The granitic rocks include typically foliated granodiorites, quartz diorites, quartz monzonites, granites; related intrusive rocks; and their metamorphosed equivalents.
• The breccia comprises angular to rounded ciasts of TTG gneisses, granites and granodiorites, with lesser amounts of amphibolite, calc-silicate rock and banded iron-formation as well as unusual dark grey to black, irregular, centimetre- to decimetre-sized ciasts that show evidence of fluidal behaviour and plastic deformation during incorporation into the breccia.
• The North-Dapaong zone, which is located in the West African Craton, migmatites, gneisses, amphibolites, granodiorites and granites are commonly found.
• The igneous rocks of the Famatinian magmatic arc are of calc-alkaline character and include gabbros, tonalites, granodiorites and trondhjemites.
• The Pampean orogen contains a magmatic belt including granodiorites, monzogranites, and volcanic rocks, all of them of calc-alkaline chemistry.
• Dedham North Granite has a compositionally highly variable suite ranging from leucogranites to granodiorites, tonalites, and quartz diorite.
• Of the Tuolumne Intrusive Suite, it is the most melanocratic of the granodiorites containing many mafic microgranular enclaves.
• Some of the rocks that can be found in abundance are ultrametamorphic, intrusive, and metasomatic complexes—that include lower Archean metagabbro, granites, diabase, granitoids, granodiorites, enderbite-charnockite, and Late Archean metagabbros.
• On the desktop there are samples of granite, plagiogranits, granodiorites, peridotites, dunitrs, serpentines, syenites, monzonites and other intrusive rocks of the Mesozoic and Cenozoic Age.
• Further south are the diorites, granites and granodiorites of the Johnston Intrusive Complex and the rhyolites of the Benton Volcanic Group which stretch from just northwest of Benton Castle west-northwestwards via Sardis and Johnston in a broken chain to the coast north of Talbenny and include Stack Rocks offshore.
• It is represented by syenites, granosyenites, monzonites, moderately alkaline granites, granodiorites.
• The central and eastern parts of the range are composed of various terrigenous rock, shists, quartzites, limestones, granodiorites, and the western part - by rocks of the middle and late Paleozoic.
• Appinites are therefore regarded as a rock series comprising hornblendites, meladiorites, diorites, but also granodiorites and granites.

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