Results 131 to 140 of about 446 (178)

Zoned Pyroxenes from Shoshonite Lavas of Lesbos, Greece: Inferences concerning Shoshonite Petrogenesis

open access: yesJournal of Petrology, 1984
Samples from several stratigraphic levels in the Miocene volcanic succession on Lesbos, Greece, contain complexly zoned clinopyroxene and feldspar phenocrysts.
Y Georgia Pe-piper
exaly   +3 more sources

Characteristics of Volcanic Rocks in the Shoshonite Province, Eastern China, and Their Metallogenesis

open access: yesActa Geologica Sinica, 1996
Abstract The shoshonite province in eastern China is characterized by extensive distribution (ca. 80000 km2) of Late Jurassic–Early Cretaceous (165–100 Ma) shoshonite series with subordinate high–K calc–alkali series. It was formed in a dominantly tensile stress field.
Wang Dezi   +5 more
exaly   +3 more sources

Miocene shoshonite volcanism in Sardinia: Implications for magma sources and geodynamic evolution of the central-western Mediterranean

open access: yesLithos, 2013
In this paper we document the existence of a Miocene shoshonite (SHO) volcanism in Northern Sardinia (Anglona). This occurrence completes the spectrum of orogenic magmas related to the subduction process which developed from the Eocene along the Palaeo ...
Claudio Natali   +2 more
exaly   +3 more sources

Water-enhanced interdiffusion of major elements between natural shoshonite and high-K rhyolite melts [PDF]

open access: yesChemical Geology, 2017
The interdiffusion of six major elements (Si, Ti, Fe, Mg, Ca, K) between natural shoshonite and a high-K rhyolite (Vulcano island, Aeolian archipelago, Italy) has been experimentally measured by the diffusion couple technique at 1200°C, pressures from 50
Maurizio Petrelli   +2 more
exaly   +2 more sources

Petrology and geochemistry of the shoshonite-hosted Skouries porphyry Cu-Au deposit, Chalkidiki, Greece

open access: yesMineralium Deposita, 2002
The Skouries porphyry Cu–Au deposit, containing an indicated reserve of 206 Mt at 0.54% Cu and 0.80 g/t Au, is hosted by at least four hypabyssal monzonite–porphyry phases.
Daniel Müller, Peter M Herzig
exaly   +2 more sources
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The shoshonite association: A review

Journal of the Geological Society of Australia, 1968
Abstract The absarokite‐shoshonite‐banakite series described from Yellowstone Park by Iddings and the ciminite‐toscanite series described from western Italy by Washington are compared. In both regions these rocks are associated with leucite‐bearing rocks, potassium‐rich trachytes and with andesitic rocks with above average potassium.
exaly   +2 more sources

The Lavras do Sul Shoshonitic Association: implications for the origin and evolution of Neoproterozoic shoshonitic magmatism in southernmost Brazil

Journal of South American Earth Sciences, 1998
Abstract The Neoproterozoic Lavras do Sul Shoshonitic Association in southernmost Brazil is related to the last stages of Brasiliano Orogeny and comprises a wide compositional range of intrusive and extrusive basic to acid rocks. It includes potassic trachybasalts, shoshonites, dacites, rhyolites, quartz diorites and monzodiorites, quartz monzonites,
E.F. De Lima, L.V.S. Nardi
openaire   +1 more source

Genesis of Mariana shoshonites: Contribution of the subduction component

Journal of Geophysical Research: Solid Earth, 2001
The Izu‐Bonin‐Mariana arc contains a unique group of shoshonitic volcanoes from along the magmatic front of this intraoceanic arc. Shoshonites are greatly enriched in incompatible elements compared to lavas typically found in primitive arc settings but have fractionations of lithophile (LIL) and high‐field strength (HFSE) incompatible elements ...
Chih‐Hsien Sun, Robert J. Stern
openaire   +1 more source

Some chemical data on members of the shoshonite association

Mineralogical Magazine, 1972
Summary A number of minerals and residual glasses from absarokites, shoshonites, and latites have been analysed by electron probe.
Germaine A. Joplin   +3 more
openaire   +1 more source

Characteristics and tectonic setting of the shoshonite rock association

Lithos, 1980
Abstract A review of the major occurrences of shoshonitic rocks suggests there is a group that is near-silica saturated, K-rich and has low iron enrichment that cannot be unambigously classified as part of calc-alkaline or alkali-basalt associations. This group is here referred to as the shoshonite rock association. The shoshonite rock association is
exaly   +2 more sources

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