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salic composition

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ε Nd ( T )–age diagram for West Transbaikalian <span class="search-highlight">composite</span> dikes and the host...
Published: 01 January 2018
Fig. 12. ε Nd ( T )–age diagram for West Transbaikalian composite dikes and the host granitoid complexes. Shaluta massif: CD 1 : 1 , basic and 2 , salic components; CD 2 : 3 , basic and 4 , salic components; 5 , composite dike of the Kurba River basin; Maksimikha site: 6 , basic and 7
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Diagrams with concordia for zircons from the rocks of <span class="search-highlight">composite</span> dikes and h...
Published: 01 January 2019
Fig. 9. Diagrams with concordia for zircons from the rocks of composite dikes and host formations of Western Sangilen. Saizyral site: a , gneissose granites of the Erzin tectonic zone, b , salic, c , basite components of the composite dike; Tavyt-Dag site: d , granites of Matut pluton, e
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TAS-diagram (SiO 2 –(Na 2 O + K 2 О)) ( The Petrographic Code, 2009 ) ( a )...
Published: 01 January 2019
zone, 2 , basite, 3 , salic components of the composite dike; Tavyt-Dag site: 4 , granites of the Matut pluton, 5 , basite, 6 , salic component of the composite dike.
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Position of biotite <span class="search-highlight">composition</span> points on the classification diagram ( a ) ...
Published: 01 January 2019
Fig. 5. Position of biotite composition points on the classification diagram ( a ) and on the diagram of the relation TiO 2 –Fe/(Fe + Mg) ( b ). Saizyral site: 1 , basite, 2 , salic components, 3 , host gneiss-plagiogranites of the Erzin tectonic zone; Tavyt-Dag site: 4 , basite, 5 , salic
Journal Article
Published: 01 December 1976
Journal of the Geological Society (1976) 132 (6): 645–666.
... the emergence of the island a compositionally bimodal population of rocks has been represented. The products of over 100 eruptions in the upper Terceira Group have been recognised. These include ignimbrites, pumice fall deposits, salic lava extrusions, strombolian scoria deposits, basaltic lava flows...
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Internal structure components of <span class="search-highlight">composite</span> dikes (dark-colored, basite, lig...
Published: 01 January 2019
Fig. 2. Internal structure components of composite dikes (dark-colored, basite, light-colored, salic components). Saizyral area (I): а , general layout of outcropping (position of the dike contact with host plagiogranite-gneiss is presented with a dashed line in the upper left corner
Journal Article
Published: 01 December 2009
Mineralogical Magazine (2009) 73 (6): 943–956.
...B. G. J. Upton; A. A. Finch; E. Słaby Abstract Ca-poor and typically Na-rich feldspar megacrysts are common associates of spinel lherzolitic and pyroxenitic xenoliths in Scottish alkalic basalts. Associated megacrysts and composite megacrysts and salic xenoliths include apatite, magnetite, zircon...
FIGURES | View All (4)
Journal Article
Published: 01 January 2018
Russ. Geol. Geophys. (2018) 59 (1): 19–40.
...Fig. 12. ε Nd ( T )–age diagram for West Transbaikalian composite dikes and the host granitoid complexes. Shaluta massif: CD 1 : 1 , basic and 2 , salic components; CD 2 : 3 , basic and 4 , salic components; 5 , composite dike of the Kurba River basin; Maksimikha site: 6 , basic and 7...
FIGURES | View All (12)
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<span class="search-highlight">Compositional</span> range of feldspars in the <span class="search-highlight">salic</span> xenolith-megacryst associatio...
Published: 01 December 2009
F ig . 2. Compositional range of feldspars in the salic xenolith-megacryst associations in Scotland ( Upton et al ., 1999 ).
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Histograms of the occurrence ( N ) of plagioclases of different <span class="search-highlight">composition</span>...
Published: 01 January 2018
Fig. 3. Histograms of the occurrence ( N ) of plagioclases of different compositions in composite dikes of the Kharitonovo, Shaluta, and Ust’-Khilok (Ust’-Khilok and Zhirim sites) massifs. Left column, basic component; right column, salic component of CD; n , number of examinations. Probability
Journal Article
Journal: GSA Bulletin
Published: 01 April 1996
GSA Bulletin (1996) 108 (4): 489–504.
.... In addition, 15 older Phanerozoic ashes, associated with other dramatic global events, have been analyzed for Ir. The Fur Formation ashes are unusually well preserved and have a wide compositional range–for example, rhyolitic, dacitic, tholeiitic and alkaline basaltic, mafic alkaline, and different salic...
Journal Article
Journal: GSA Bulletin
Published: 01 December 1979
GSA Bulletin (1979) 90 (12): 1100–1110.
...DONNIE F. PARKER; FRED W. McDOWELL Abstract Volcanic rocks of the Davis and Barrilla Mountains constitute the largest contiguous segment of the mid-Cenozoic volcanic field of Trans-Pecos Texas. Salic volcanic rocks form a silica-oversaturated series ranging in composition from trachyte...
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Some accessory minerals in glasses from the Popigai impact tuffisites.  A  ...
Published: 01 June 2006
-1/3. Dark fields above and below are composed of salic K-Na-glass; C — fine emulsive spherule of the products of shock melting and decomposition of zircon, with drops of melt inclusions. Particle 0504-2/4 of argillized glass; D — monazite grains (M) and femic mineral “shadow” composed
Journal Article
Journal: GSA Bulletin
Published: 01 March 1984
GSA Bulletin (1984) 95 (3): 337–349.
... basaltic shields and intermediate to salic peralkaline composite domes, flows, and central volcanoes that are associated with extensional structures in the underlying basement. New K-Ar and fission-track dates (45) and Rb-Sr and Sr isotope analyses (12) from the Mount Edziza Volcanic Complex are reported...
Journal Article
Journal: Geology
Published: 01 April 1974
Geology (1974) 2 (4): 187–190.
... to 400 ppm and 50 to 80 ppm for the more salic whole-rock and residual glass specimens. The behavior of these elements largely reflects the separation of large amounts of phenocrystic plagioclase. Sr content closely follows that of calcium. More sodic plagioclase exhibits a greater absolute affinity...
Journal Article
Published: 01 April 1973
Canadian Journal of Earth Sciences (1973) 10 (4): 538–550.
..., matrix percent, and sorting imply vent areas to the west and south of the Kakagi Lake area.The rocks are calc-alkaline rather than tholeiitic in lineage, poor in K 2 O, particularly the most silicic. Fragments are more salic and depleted in FeO and MgO relative to their matrix.Thickness and lack...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1969
GSA Bulletin (1969) 80 (7): 1283–1310.
... phonolitic rocks. The composition of the parental basalt remained nearly constant throughout the history of the volcanoes, and intermediate and salic rocks increased in volume and frequency of occurrence during their growth. It is suggested that on Saint Helena the increasing production with time...
Journal Article
Journal: GSA Bulletin
Published: 01 August 1964
GSA Bulletin (1964) 75 (8): 741–744.
... the different behavior of these minerals under shearing stress. The normal metadolerite has 58 per cent salic, and 42 per cent femic minerals. An analyzed dark layer of the mylonite has 60 per cent femic minerals, whereas an analyzed light layer shows 86 per cent salic minerals. Pneumatolytic alteration...
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REE patterns in the basic ( a ) and <span class="search-highlight">salic</span> ( b ) members of the bimodal asso...
Published: 01 February 1998
Fig. 5. REE patterns in the basic ( a ) and salic ( b ) members of the bimodal association of the Tamir VTS (chondrite composition from [ 21 ]). a : 1 – trachybasalts, 2 – trachyandesite-basalts, 3 – gabbroids, 4 – diorites and monzodiorites; b : 5 – trachytes and alkali trachydacites
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Occurrence frequency histograms of plagioclase of different <span class="search-highlight">compositions</span> (m...
Published: 01 January 2019
Fig. 3. Occurrence frequency histograms of plagioclase of different compositions (mol. % An) in composite dikes of Western Sangilen: a , basite, b , salic components. The curves of probability density distribution: 1 , Tavyt-Dag dike; 2 , Saizyral dike. The composition of rock-forming