Abstract
Late Precambrian granitoid rocks occurring within a 44,000 km2 area of the western Arabian Shield are subdivided on the basis of geology and petrology into older (820 to 715 Ma) and younger (686 to 517 Ma) assemblages. The older assemblage contains major complexes which can be assigned to either one of a granodioritic or trondhjemitic petrologic association. The earliest granitoid rocks are trondhjemitic tonalites (trondhjemite association), depleted in Ba, Ce, F, La, Li, Nb, Rb, Y and Zr compared to granitoids of the slightly younger granodiorite association, which are related to a calcic, calc-alkaline suite of rocks ranging in composition from gabbro through monzogranite. The plutonic rocks of the older assemblage were probably emplaced in the cores of contemporary island arcs.
The younger plutonic assemblage is dominated by three, geochemically distinct, coeval granitic associations: the alkali granite, alkali-feldspar granite and monzogranite associations. The alkali granite association is composed of perthite granites (alkali granites and genetically related alkali-feldspar granites). Rocks of this association are marginally peralkaline or metaluminous and are characterized by low contents of Ba, Co, Li, Rb, Sc and Sr, and high contents of Be, Cu, F, REE, Nb, Sn, Y, Zn and Zr. The alkali-feldspar granite association is mainly composed of alkali-feldspar granites and syenogranites. Rocks of this association are marginally peraluminous or metaluminous and contain low Ba, Sr, and high F, Rb, Sn, Th and U. The monzogranite association consists mainly of monzogranites and granodiorites. Rocks of this association are peraluminous or marginally metaluminous and have the highest contents of Ba, Cu, Co, Li, Sc, Sr, Ta, and V, and the lowest contents of REE, Nb, Rb, Sn, Th, U, Y, Zn and Zr of the three granitic associations.
These voluminous granitic magmas, together with the felsic component of a coeval sequence of bimodal volcanic rocks, are partial melts of the earlier island arc terrain produce during a prolonged fusion event. Subsolvus, ‘highca’ granites of the monzogranite association have I-type features and represent partial melts of previously unfused crust, while ‘low-Ca’ perthite granites of the alkali granite and alkali-feldspar granite associations have A-type features and represent partial melts of previously fused crust.
This type of petrogenetic model can account for much of the petrologic diversity of the Pan-African granitic terrain of the Arabian Shield.
Similar content being viewed by others
References
Abdel-Monem AA, Al-Shanti AM, Radain AA (1982) Rb-Sr dating and petrochemistry of some granite bodies, west-central Saudi Arabia. Precambrian Res 16: No. 4, A3
AGI (1980) Glossary of Geology—0Second Edition. American Geological Institute, Falls Church, Virginia, pp 749
Aleinikoff JN, Stoeser DB, U-Pb zircon geochronology of alkaline and peralkaline granites of the Arabian Shield. Saudi Arabian Deputy Ministry for Mineral Resources Open-File Report (in prep)
Al-Shanti AM, Abdel-Monem AA (1982) Rb-Sr dating and petrochemistry of Umm Gerad granitic rocks, western Saudi Arabia. Precambrian Res: 16, No 4, A6
Arth JG (1979) Some trace elements in trondhjemites—their implications for magma genesis and paleotectonic setting. In: Barker F (ed), Trondhjemites, dacites and related rocks. Elsevier 123–132
Arth JG, Barker F (1976) Rare earth partitioning between hornblende and dacitic liquid and implications for the genesis of trondhjemitic-tonalitic magmas Geology 4:534–536
Arth JG, Hanson GN (1975) Geochemistry and origin of the early Precambrian crust of northeastern Minnesota. Geochim Cosmochim Acta 39:325–362
Atherton MP, McCourt WJ, Sanderson LM, Taylor WP (1979) The geochemical character of the segmented Peruvian coastal batholith and associated volcanics. In: Atherton MP, Tarney J (eds) Origin of granitic batholiths: geochemical evidence. Shiva Publishing, Orpington, Kent 45–64
Bakor AB, Gass IG, Neary CR (1976) Jabal al Wask, NW Saudi Arabia: an Ecocambrian back-arc ophiolite. Earth Planet Sci Lett 30:1–9
Barker F (1979) Trondhjemite: definition, environment and hypothesis of origin. In: Barker F (ed) Trondhjemites, dacites and related rocks. Elsevier, pp 1–12
Barker F, Arth JG (1976) Generation of trondhjemitic-tonalitic liquids and Archean bimodal trondhjemite-basalt suites. Geology 4:596–600
Bokhari FY, Kramers JD (1981) Island arc character and late Precambrian age of volcanics at Wadi Shwas, Hijaz, Saudi Arabia: geochemical and Sr and Nd isotopic evidence. Earth Planet Sci Lett 54:409–422
Brown GC (1980) Calc-alkaline magma genesis: the Pan-African contribution to crustal growth? Inst Applied Geol King Abdulaziz University, Jeddah, Bull 4: 3, 19–29
Brown GC, Hennessy J (1978) The initiation and thermal diversity of granite magmatism. Phil Trans R Soc London Ser A 288:631–643
Brown GC (1982) Calc-alkaline intrusive rocks: their diversity, evolution and relation to volcanic arcs. In: Thorpe RS (ed) Andesites: John Wiley and Sons 437–461
Calvez JY, Alsac C, Delfour J, Kemp J, Pellaton C (1983 a) Geologic evolution of western central and eastern parts of the northern Precambrian Shield, Kingdom of Saudi Arabia. Unpublished Rept Saudi Arabian Deputy Ministry of Mineral Resources
Calvez JY, Pellaton C, Alsac C, Tegyey M (1983 b) Geochronology and geochemistry of plutonic rocks in the Umm Lajj and Jabal al Buwanah areas: Unpubl Rept Saudi Arabian Deputy Ministry for Mineral Resources
Camp V, Geologic map of the Umm al Birak quadrangle, sheet 23D, Kingdom of Saudi Arabia (1:250,000). Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map series (in press a)
Camp V, Island arcs and their role in the evolution of the western Arabian Shield Geol. Soc America Bull (in press b)
Chappell BW, White AJR (1974) Two contrasting granite types. Pac Geol 8:173–174
Claesson S, Pallister JS, Tatsumoto M (1984) Samarium — neodymium data on two late Proterozoic ophiolites of Saudi Arabia and implications for crustal and mantle evolution. Contrib Mineral Petrol 85:244–252
Clark MD (1981) Geologic map of the Al Hamra' quadrangle, sheet 23C: Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map series, GM-49A (1:250,000)
Collins WJ, Beams SD, White AJR, Chappell BW (1982) Nature and origin of A-type granites with particular reference to southeastern Australia Contrib Mineral Petrol 80:189–200
Darbyshire DPF, Jackson NJ, Ramsay CR, Roobol MJ (1983) Rb-Sr isotope study of latest Proterozoic volcano-sedimentary belts in the central Arabian Shield. J Geol Soc London 140:203–213
Dodge FCW (1979) The Uyaijah ring structure, Kingdom of Saudi Arabia. US Geol Surv PP 774–E:17
Drysdall AR, Jackson NJ, Douch CJ, Ramsay CR, Hackett Rare metal mineralization related to Precambrian alkali granites in the Arabian Shield. Econ Geol (in press)
Duyverman HJ, Harris NBW, Hawkesworth CJ (1982) Crustal accretion in the Pan African: Nd and Sr isotope evidence from the Arabian Shield: Earth Planet Sic Lett 59:315–326
Faure G, Powell JL (1972) Strontium isotope geology. Springer, Berlin, pp 188
Fitches WR, Graham RH, Hussein IM, Ries AC, Shackleton RM, Price RC (1983) The Late proterozoic ophiolite of Sol Hamed, NE Sudan. Precambrian Res 19:385–411
Fleck RJ, Greenwood WR, Hadley DG, Anderson RE, Schmidt DL (1980) Age and evolution of the southern part of the Arabian Shield. Inst Applied Geol King Abdulaziz University (Jeddah) Bull 3:1–17
Gass IG (1977) The evolution of the Pan-African crystalline basement in Ne Africa and Arabia. J Geol Soc London 134:129–138
Gass IG (1979) Evolutionary model for the Pan African crystalline basement. Inst Applied Geol, King Abdulaziz University (Jeddah) Bull 3:11–29
Gass IG (1981) Pan-African (Upper Proterozoic) plate tectonics of the Arabian-Nubian Shield. In: Kroner A (ed) Precambrian plate tectonics: Elsevier, Amsterdam, pp 387–405
Gill JB, Stork AL (1979) Miocene low-K dacites and trondhjemites of Fiji. In: Barker F (ed) Trondjemites, dacites and related rocks: Elsevier, Amsterdam, pp 629–649
Greenberg JK (1981) Characteristics and origin of Egyptian younger granites. Geol Soc Am Bull (Part II) 92:749–840
Greenwood WR, Brown GC (1973) Petrology and chemical analyses of selected plutonic rocks from the Arabian Shield, Kingdom of Saudi Arabia. Saudi Arabian Directorate General of Mineral Resources Bull 9, p 9
Greenwood WR, Hadley DG, Anderson RE, Fleck RJ, Schmidt DL (1976) Late Proterozoic cratonization in southwestern Saudi Arabia. Phil Trans R Soc London Ser A 280:517–527
Healy JH, Money WD, Blank HR, Gettings E (1980) Deep structure of the Arabian Shield from the 1978 USGS/DGMR seismic refraction profile: Fac Earth Sci King Abdulaziz University (Jeddah), Res Ser 13:136–137
Hildreth W (1981) Gradients in silicic magma chambers: implications for lithospheric magmatism: J Geophys Res 86:No 811, 10153–10192
Hine R, Mason DR (1978) Intrusive rocks associated with porphyry copper mineralization. New Britain, Papua New Guinea. Econ Geol 73:749–760
Jackaman B (1972) Genetic and environmental factors controlling the formation of the massive sulfide deposits of Wadi Bidah and Wadi Wassat: Saudi Arabian Directorate General of Mineral Resources Tech Rec TR-1972-1: p 243
Jackson NJ, Douch CJ, Odell J, Bedawi H, Al-Hazmi H, Pegram E, Walsh JN, Late Precambrian granitoid plutonism and associated mineralization in the central Hijaz: Fac Earth Sci, King Abdulaziz University (Jeddah) Bull 6: (in press)
Jackson NJ, Ramsay CR (1980) Time-space relationships of Upper Precambrian volcanic and sedimentary units in the central Arabian Shield. J Geol Soc. London 137:717–728
Kemp J, Pellaton C, Calvez JY (1982) eochronological investigations and geological history in the Precambrian of northwestern Saudi Arabia. Unpublished Rept. Saudi Arabian Deputy Ministry for Mineral Resources
Kemp J, Pellaton C, Calvez JY (1982) Cycles in the chelogenic evolution of the Precambrian Shield in part of northwestern Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources PP. Series 1:29–41
Lambert R St J, Holland JG (1974) Yttrium geochemistry applied to petrogenesis utilizing calcium-yttrium relationships in minerals and rocks: Geochim Cosmochim Acts 38:1393–1414
Loiselle MC, Wones DR (1979) Characteristics of anorogenic granites: Geol Soc Am AGM (1979) Abstr with Progr: 539
Nakamura N (1974) Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous and ordinary chondrites: Geochim Cosmochim Acta 38:575–775
Nasseef AO, Gass IG (1977) Granitic and metamorphic rocks of the Ta'if area, western Saudi Arabia. Geol Soc Am Bull 88:1721–1730
Nasseef MO, Macdonald R, Gass IG The Jabal Thurwah Upper Proterozoic ophiolite complex, western Saudi Arabia. J Geol Soc London (in press)
Neary CR, Gass IG, Cavanagh BJ (1976) Granitic association of northeastern Sudan: Geol Soc Am Bull 87:1501–1512
Pellaton C (1979) Geologic map of the Yanbu al Bahr quadrangle, sheet 24C. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map Series GM-48A (1:250,000)
Pellaton C (1981) Geologic map of the Al Madinah quadrangle, sheet 24D. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map Series, GM-52A (1:250,000)
Pellaton C (1982) Geologic map of the Jabal Al Buwanah quadrangle, sheet 24B. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map Series, GM-62C (1:250,000)
Peterman ZE (1979) Strontium isotope geochemistry of late Archean to Cretaceous tonalites and trondhjemites. In: Barker F (ed) Trondhjemites, dacites and related rocks: Elsevier, Amsterdam, 133–147
Phelps D (1979) Petrology, geochemistry and origin of the Sparta quartz diorite trondhjemite complex, northwestern Oregon. In: Barker F (ed) Trondhjemites, dacites and related rocks. Elsevier, Amsterdam, 547–579
Ramsay CR (1982) Geology and mineral resource potential of Pan-African granitoid rocks, northern Midyan region. Unpubl Rept Saudi Arabian Deputy Ministry for Mineral Resources
Ramsay CR, Drysdall AR, Clark MD, Odell J, Felsic plutonic rocks of the Midyan Region, Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Bull (in press)
Roobol MJ, Ramsay CR, Jackson NJ, Darbyshire DPF (1983) Late Proterozoic lavas of the central Arabian Shield — evolution of an ancient volcanic arc system in the Arabian Shield. J Geol Soc London 140:185–202
Skiba WJ (1980) The form and evolution of late Precambrian plutonic rocks in the Jiddah-Rabigh-Wadi Al-Qahah area, Saudi Arabia. Inst Applied Geol King Abdulaziz University (Jeddah) Bull 3: v3, 105–120
Stoeser DB, Stacey JS, Greenwood WR, Fisher LB, U/Pb zircon geochronology of the southern portion of the Nabitah mobile belt and Pan African continental collision in the Saudi Arabian Shield. Saudi Arabian Deputy Ministry for Mineral Resources Technical Record USGS-TR-04 (in press)
Stoeser DB, Elliott JE (1980) Post-orogenic peralkaline and calcalkaline granites and associated mineralization of the Arabian Shield, Kingdom of Saudi Arabia. Inst Applied Geol, King Abdulaziz University (Jeddah) Bull 3:1–23
Streckeisen A (1976) To each plutonic rock its proper name. Earth Science Reviews 12:1–33
Tarney J, Saunders AD (1979) Trace element constraints on the origin of cordilleran batholiths. In: Atherton MP, Tarney J (eds) Origin of granitic batholiths: geochemical evidence: Shiva Publishing, Orpington, Kent 90–105
Tuttle OF, Bowen NL (1958) Origin of granite in the light of experimental studies in the system (NaAl) Si3O8-(KAl)Si3O8-SiO2-H2O. Geol Soc Am Mem 74:1–53
Walsh JN (1980) The simultaneous determination of major and trace constituents of silicate rocks using inductively coupled plasma spectrometry. Spectrochem Acta 35B:107–111
Walsh JN, Buckley F, Barker J (1981) The sumultaneous determination of the rare earth elements in rocks using inductively coupled plasma source spectrometry. Chem Geol 33:141–153
Winkler HGF (1967) Petrogenesis of metamorphic rocks: Springer, Berlin Heidelberg New York, p 237
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Jackson, N.J., Walsh, J.N. & Pegram, E. Geology, geochemistry and petrogenesis of late Precambrian granitoids in the Central Hijaz Region of the Arabian Shield. Contr. Mineral. and Petrol. 87, 205–219 (1984). https://doi.org/10.1007/BF00373054
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00373054