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N. Agron, Y. Bentor (1981)
The Volcanic Massif of Biq'at Hayareah (Sinai-Negev): A Case of Potassium MetasomatismThe Journal of Geology, 89
(1990)
A mechanism of dyke segmentation in fractured host rock
G. Jarrar, H. Wachendorf, G. Saffarini (1992)
A late Proterozoic bimodal volcanic/subvolcanic suite from Wadi Araba, southwest JordanPrecambrian Research, 56
A. Kröner, M. Eyal, Y. Eyal (1990)
Early Pan-African evolution of the basement around Elat, Israel,and the Sinai Peninsula revealed by single-zircon evaporation dating, and implications for crustal accretion ratesGeology, 18
T. Irvine, W. Baragar (1971)
A Guide to the Chemical Classification of the Common Volcanic RocksCanadian Journal of Earth Sciences, 8
(1988)
1988).Bimodal dike swarms in the North EasternDesert of Egypt; significance for the origin of late Precambrian `A-type' granites in northern Afro-Arabia
M. Bas, R. Maitre, A. Streckeisen, B. Zanettin (1986)
A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica DiagramJournal of Petrology, 27
(1959)
The geology and petrography of the Amram mountains
William Collins, S. Beams, A. White, B. Chappell (1982)
Nature and origin of A-type granites with particular reference to southeastern AustraliaContributions to Mineralogy and Petrology, 80
R. Creaser, R. Price, R. Wormald (1991)
A-type granites revisited: Assessment of a residual-source modelGeology, 19
A. Reymer, G. Schubert (1984)
Phanerozoic addition rates to the continental crust and crustal growthTectonics, 3
(1996)
Geochemical and isotopic (O, Nd, Pb and Sr) constraints on A-type granite petrogenesis based on the Topsails Igneous Suite
M. Zimmer, A. Kröner, K. Jochum, T. Reischmann, W. Todt (1995)
The Gabal Gerf complex: A precambrian N-MORB ophiolite in the Nubian Shield, NE AfricaChemical Geology, 123
(2000)
Petrogenesis and tectonic setting of Neoproterozoic granites from the Northernmost Arabian Shield
(2000)
Petrogenesis and tectonic setting of Neoproterozoic granites from the Northernmost Arabian Shield, SW Jordan
M. Beyth, R. Stern, R. Altherr, A. Kröner (1994)
The Late Precambrian Timna igneous complex, Southern Israel: Evidence for comagmatic-type sanukitoid monzodiorite and alkali granite magmaLithos, 31
A. Moghazi, T. Andersen, G. Oweiss, A. Bouseily (1998)
Geochemical and Sr–Nd–Pb isotopic data bearing on the origin of Pan-Africangranitoids in the Kid area, southeast Sinai, EgyptJournal of the Geological Society, 155
Z. Garfunkel (1989)
Tectonic setting of phaneroozoic magmatism in IsraelIsrael Journal of Earth Sciences, 38
(1999)
The youngest igneous event in the crystalline basement of the Arabian±Nubian Shield, Timna igneous complex
D. Almond (1987)
The crustal evolution of the Arabo-Nubian Massif with special reference to the Sinai PeninsulaPrecambrian Research, 34
M. Stein, A. Hofmann (1992)
Fossil plume head beneath the Arabian lithosphereEarth and Planetary Science Letters, 114
(1994)
Petrochemistry of dolerite dykes from Mount Timna, southern Israel; implications for plate tectonic setting
(1995)
The geochemistry of dykes and their host rocks from the latest stages in the Pan African orogeny
A. Mushkin, O. Navon, L. Halicz, A. Heimann, G. Woerner, M. Stein (1999)
Geology and geochronology of the Amram Massif, southern Negev Desert, IsraelIsrael Journal of Earth Sciences, 48
G. Jarrar (2001)
The youngest Neoproterozoic mafic dyke suite in the Arabian Shield: mildly alkaline dolerites from South Jordan – their geochemistry and petrogenesisGeological Magazine, 138
S. Turner, J. Foden, R. Morrison (1992)
Derivation of some A-type magmas by fractionation of basaltic magma: an example from the Padthaway R
(1959)
The geology and petrography of the Amram mountains, southern Israel
R. Black, J. Liégeois (1993)
Cratons, mobile belts, alkaline rocks and continental lithospheric mantle: the Pan-African testimonyJournal of the Geological Society, 150
M. Ghiorso, R. Sack (1995)
Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressuresContributions to Mineralogy and Petrology, 119
C. Devey, K. Cox (1987)
Relationships between crustal contamination and crystallisation in continental flood basalt magmas with special reference to the Deccan Traps of the Western Ghats, IndiaEarth and Planetary Science Letters, 84
A. Mcguire, R. Stern (1993)
Granulite xenoliths from western Saudi Arabia: the lower crust of the late Precambrian Arbian-Nubian ShieldContributions to Mineralogy and Petrology, 114
M. Bielski, E. Jäger, G. Steinitz (1979)
The geochronology of Iqna Granite (wadi Kid pluton), Southern SinaiContributions to Mineralogy and Petrology, 70
T. Reischmann, A. Kröner, A. Basahel (1982)
Petrography, geochemistry and tectonic setting of metavolcanic sequences from the Al-Lith area, southwestern Arabian shieldPrecambrian Research, 16
M. Stein, O. Navon, R. Kessel (1997)
Chromatographic metasomatism of the Arabian—Nubian lithosphereEarth and Planetary Science Letters, 152
H. Fujimaki (1986)
Partition coefficients of Hf, Zr, and REE between zircon, apatite, and liquidContributions to Mineralogy and Petrology, 94
(1995)
1995).The geochemistry of dykes and their host rocks from thelatest stages inthePanAfricanorogeny,AmramandElatmassifs, southern Israel
G. Chazot, H. Bertrand (1995)
Genesis of silicic magmas during tertiary continental rifting in YemenLithos, 36
A. Parker, P. Rickwood, D. Tucker (1990)
Mafic dykes and emplacement mechanisms
(1980)
Contribution to the geology of the Precambrian of the Elat area
D. DePaolo (1981)
Trace element and isotopic effects of combined wallrock assimilation and fractional crystallizationEarth and Planetary Science Letters, 53
(1980)
Katherina Pluton; the outlines of a petrologic framework
S. Turner (1996)
Petrogenesis of the late-Delamerian gabbroic complex at Black Hill, South Australia: Implications for convective thinning of the lithospheric mantleMineralogy and Petrology, 56
A. H.
The Evolution of the Igneous RocksNature, 124
(1988)
Bimodal dike swarms in the North EasternDesert of Egypt ; significance for the origin of late Precambrian ` A - type ' granites in northern Afro - Arabia
R. Altherr, F. Henjes‐Kunst, A. Baumann (1990)
Asthenosphere versus lithosphere as possible sources for basaltic magmas erupted during formation of the Red Sea: constraints from Sr, Pb and Nd isotopesEarth and Planetary Science Letters, 96
(1980)
Ferric±ferrous equilibrium in silicate liquids at 1 bar
(1996)
The age of the quartz monzodiorite, the youngest plutonic intrusion in the Timna igneous complex
H. Nekvasil, A. Simon, D. Lindsley (2000)
Crystal Fractionation and the Evolution of Intra-plate hy-normative Igneous Suites: Insights from their FeldsparsJournal of Petrology, 41
M. Stein, S. Goldstein (1996)
From plume head to continental lithosphere in the Arabian–Nubian shieldNature, 382
M. Stein, A. Hofmann (1994)
Mantle plumes and episodic crustal growthNature, 372
J. Whalen, Kenne Currie, B. Chappell (1987)
A-type granites: geochemical characteristics, discrimination and petrogenesisContributions to Mineralogy and Petrology, 95
G. Eby (1992)
Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implicationsGeology, 20
(1998)
Geochemical and Sr±Nd±Pb isotopic data bearing on the origin of Pan-African granitoids in the Kid area
Richard Volkert, M. Feigenson, L. Patiño, J. Delaney, A. Drake (2000)
Sr and Nd isotopic compositions, age and petrogenesis of A-type granitoids of the Vernon Supersuite, New Jersey Highlands, USALithos, 50
J. Whalen, G. Jenner, F. Longstaffe, Francine Robert, C. Gariépy (1996)
Geochemical and Isotopic (O, Nd, Pb and Sr) Constraints on A-type Granite Petrogenesis Based on the Topsails Igneous Suite, Newfoundland AppalachiansJournal of Petrology, 37
(2000)
Sr and Nd isotopic compositions, age and petrogenesis of A-type granitoids of the Vernon Supersuite
(1990)
Asthenosphere versus lithosphere as possible sources for basaltic magmas erupted during the formation of the Red Sea: constraints from Sr
W. Nash, H. Crecraft (1985)
Partition coefficients for trace elements in silicic magmasGeochimica et Cosmochimica Acta, 49
(1987)
Ultra-basic xenoliths in Cenozoic and Mesozoic volcanic rocks in Israel
(1979)
The geochronology of Iqna Granite
R. Kessel, M. Stein, O. Navon (1998)
Petrogenesis of late Neoproterozoic dikes in the northern Arabian–Nubian Shield: Implications for the origin of A-type granitesPrecambrian Research, 92
(1994)
Late-medieval glass manufacture in the Eischsfeld region
(1971)
Late lower Cambrian trilobites from the Timna area and Har'Amram (southern Negev, Israel)
V. Camp, M. Roobol (1992)
Upwelling asthenosphere beneath western Arabia and its regional implicationsJournal of Geophysical Research, 97
(1999)
History and paleogeography during the Pan-African orogen to stable platform transition: reappraisal of the evidence from the Elat area and the northern Arabian± Nubian Shield
(1970)
The tectonics of the western margin of the southern Arava
(1982)
Evolution stages of the Arab±Nubian Massif in the Sinai
B. Landenberger, W. Collins (1996)
Derivation of A-type Granites from a Dehydrated Charnockitic Lower Crust: Evidence from the Chaelundi Complex, Eastern AustraliaJournal of Petrology, 37
R. Stern, D. Gottfried (1986)
Petrogenesis of a Late Precambrian (575–600 Ma) bimodal suite in Northeast AfricaContributions to Mineralogy and Petrology, 92
(1999)
The Pan-African plume event and growth of Gondwana
R. Sack, I. Carmichael, M. Rivers, M. Ghiorso (1981)
Ferric-ferrous equilibria in natural silicate liquids at 1 barContributions to Mineralogy and Petrology, 75
N. Nakamura (1974)
Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous and ordinary chondritesGeochimica et Cosmochimica Acta, 38
G. Eby (1990)
The A-type granitoids: A review of their occurrence and chemical characteristics and speculations on their petrogenesisLithos, 26
T. Dunn, Cüneyt Şen (1994)
Mineral/matrix partition coefficients for orthopyroxene, plagioclase, and olivine in basaltic to andesitic systems: A combined analytical and experimental studyGeochimica et Cosmochimica Acta, 58
J. Marsh (1989)
Geochemical constraints on coupled assimilation and fractional crystallization involving upper crustal compositions and continental tholeiitic magmaEarth and Planetary Science Letters, 92
(1989)
Tectonic setting of Phanerozoic magmatism in Israel
The (∼550–530 Ma) alkaline magmatic suite of the Amram Massif, southern Israel, was emplaced during the transition from an orogenic to an intra-plate tectonic setting in the northeastern Arabian–Nubian Shield (ANS). The suite ranges from 45·6 to 78·8 wt % SiO 2 , and consists of rhyolites, alkali quartz syenites, quartz syenites, monzonites, and co-magmatic mafic to felsic alkaline dikes. These rocks define a continuous chemical evolutionary trend and reveal a correlation between decreasing stratigraphic age and increasing silica content. The felsic members of the suite display A-type characteristics and are genetically linked through fractionation to the more mafic ones. Moderately positive initial εNd values (+2 ± 0·5), low initial 87 Sr/ 86 Sr values (0·7036 ± 2), high MgO and Fe 2 O 3 concentrations (4·10–8·95 and 10·0–12·5 wt %, respectively) and relatively flat rare earth element patterns ((La/Yb) n = 6·4 ± 0·9) in the Amram mafic dikes (45·6–49·5 wt % SiO 2 ), suggest their derivation from the sub-continental lithospheric mantle, above the garnet stability zone. The MELTS program was used to quantitatively model the chemical evolution of the suite. Extensive anhydrous fractionation (>90%), of plagioclase, alkali-feldspar, clinopyroxene, olivine, and minor Ti-magnetite and apatite from parental mafic magmas, represented by the Amram mafic dikes, produced the rhyolitic compositions as well as the intermediate members of the suite. This suggests the presence of a large unexposed body of cumulate rocks at depth, as well as fusion of a large source-region (equivalent to an ∼5 km layer) in the lithospheric mantle. Regarded as a representative example for similar A-type outcrops in this region, this petrogenetic model further suggests that Neoproterozoic–Early Cambrian A-type magmatism in the northeastern ANS represents a significant post-orogenic addition of mantle-derived material to the juvenile crust. This magmatic episode was of a similar magnitude to that of the Cenozoic, extension-related, alkaline volcanism of the Arabian plate. Key words
Journal of Petrology – Oxford University Press
Published: May 1, 2003
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