Skip to main content
Log in

Petrology of a portion of the Eastern Peninsular Ranges mylonite zone, Southern California

  • Published:
Contributions to Mineralogy and Petrology Aims and scope Submit manuscript

Abstract

Peraluminous and metaluminous plutonic rocks of the Peninsular Ranges batholith near Borrego Springs in southern California were mylonitized in the large shear zone known as the eastern Peninsular Ranges mylonite zone (EPRMZ). Accompanying mylonitization in this portion of the EPRMZ was metamorphism at intermediate-low-pressure amphibolite-facies conditions. Deformation in the zone overlapped in time with Cretaceous intrusion of the batholith. In the San Ysidro Mountain — Pinyon Ridge area, four north-south trending zones of differing intensity of deformation have been defined; from east to west the degree and style of deformation gradually change from undeformed or weakly deformed rocks to strongly mylonitized rocks.

Electron microprobe analysis shows that recrystallized hornblende, biotite, and plagioclase are variable in composition, probably reflecting a range of metamorphic conditions accompanying deformation. Comparison of mineral compositions with those from mafic schists of Vermont suggests conditions ranged from andalusite-staurolite through sillimanite-muscovite grades as defined for pelitic rocks. Stability of muscovite+quartz in mylonite assemblages and lack of remelting of granitic rocks indicate that temperature did not exceed about 650° C during mylonitization and lithostatic pressure did not exceed about 5 kbar. Over time, any given rock volume experienced a range of temperature, lithostatic pressure, and perhaps fluid pressure and differential stress.

Mineral reactions in the zone involved hydration, requiring introduction of water. The possibility of large-scale migration of K and Fe is suggested by whole-rock chemical data. Brittle and ductile deformation features are closely associated in one part of the EPRMZ. The combined evidence suggests the presence of a pore fluid with fluid pressure close to lithostatic pressure. Short periods of low fluid pressure and possible high differential stress cannot be ruled out.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Albee AL, Ray L (1970) Correction factors for electron probe microanalysis of silicates, oxides, carbonates, phosphates, and sulfates. Anal Chem 42:1408–1414

    Google Scholar 

  • Anderson JR (1977) The polymetamorphic sequence in the Paleozoic rocks of northern Vermont: a new approach using metamorphic veins as petrologic and structural markers. Unpubl PhD thesis, California Inst Technology

  • Anderson JR (1980) A study of mylonitic rocks from major fault zones (report). US Geol Surv Open-file Report 80-1154

  • Anderson JR (1982) A study of mylonitic rocks from major fault zones (summary of report). US Geol Surv Open-file Report 82-65:399–400

    Google Scholar 

  • Bence AE, Albee AL (1968) Empirical correction factors for the electron mircroanalysis of silicates and oxides. J Geol 76:382–403

    Google Scholar 

  • Bohlen SR, Essene EJ, Hoffman KS (1980) An update on feldspar and oxide thermometry in the Adirondack Mountains, New York. Geol Soc Am Bull, Part I 91:110–113

    Google Scholar 

  • Brown PE, Essene EJ, Kelly WC (1978) Sphalerite geobarometry in the Balmat-Edwards district, New York. Am Mineral 63:250–257

    Google Scholar 

  • Champion DE, Albee AL, Chodos AA (1975) Reproducibility and operator bias in a computer-controlled system for quantitative electron microprobe analysis. Microbeam Anal Soc Proc Annu Conf:55A–55F

  • Chodos AA, Albee AL, Gancarz AJ, Laird J (1973) Optimization of computer-controlled quantitative analysis of minerals. Microbeam Anal Soc Proc Annu Conf:45A–-45C

  • Christie JM, Ord A (1980) Flow stress from microstructures of mylonites: example and current assessment. J Geophys Res 85:6253–6262

    Google Scholar 

  • Davis ME (1981) Petrology, structure, and geochemistry of a portion of the Carthage-Colton mylonite zone, South Edwards quadrangle, NW Adirondacks. Unpubl MA thesis, SUNY-Binghamton

    Google Scholar 

  • Davis ME, Anderson JR (1983) Metamorphism accompanying mylonitization of hornblende-quartz syenite, Carthage-Colton mylonite zone, NW Adirondacks. Geol Soc Am Abstr with Program 15:141

    Google Scholar 

  • Evans BW (1965) Application of a reaction-rate method to the breakdown of muscovite plus quartz. Am J Sci 263:647–667

    Google Scholar 

  • Fraser DM (1931) Geology of the San Jacinto quadrangle south of San Gorgonio Pass. Calif Div Mines Geol Bull 27:494–540

    Google Scholar 

  • Holdaway MJ (1971) Stability of andalusite and the aluminum silcate phase diagram. Am J Sci 271:97–131

    Google Scholar 

  • Laird J (1977) Phase equilibria in mafic schist and the polymetamorphic history of Vermont. Unpubl PhD thesis, California Inst Technology

  • Laird J, Albee AL (1981a) High pressure metamorphism in mafic schist from northern Vermont. Am J Sci 281:97–126

    Google Scholar 

  • Laird J, Albee AL (1981b) Pressure, temperature, and time indicators in mafic schist: their application to reconstructing the polymetamorphic history of Vermont. Am J Sci 281:127–175

    Google Scholar 

  • Larsen ES (1948) Batholith and associated rocks of Corona, Elsinore, and San Luis Rey quadrangles, southern California. Geol Soc Am Mem 29

  • Shapiro L (1967) Rapid analysis of rocks and minerals by a single solution method. US Geol Surv Prof Paper 575B:B187–191

    Google Scholar 

  • Shapiro L, Brannock WW (1962) Rapid analysis of silicate, carbonate and phosphate rocks. US Geol Surv Bull 1144 A

  • Sharp RV (1966) Ancient mylonite zone and fault displacements in the Peninsular Ranges of southern California. Geol Soc Am Spec Paper 101:333

    Google Scholar 

  • Sharp RV (1967) San Jacinto fault zone in the Peninsular Ranges of southern California. Geol Soc Am Bull 78:705–730

    Google Scholar 

  • Sharp RV (1979) Some characteristics of the eastern Peninsular Ranges mylonite zone. US Geol Surv Open-file Report 79-1239:258–267

  • Sibson RH (1980) Transient discontinuities in ductile shear zones. J Struct Geol 2:165–171

    Google Scholar 

  • Stoddard EF (1980) Metamorphic conditions at the northern end of the northwest Adirondack Lowlands. Geol Soc Am Bull, Part I 91:100–102

    Google Scholar 

  • Theodore TG (1970) Petrogenesis of mylonites of high metamorphic grade in the Peninsular Ranges of southern California. Geol Soc Am Bull 81:435–450

    Google Scholar 

  • Tuttle OF, Bowen NL (1958) Origin of granite in light of experimental studies in the system NaAlSi3O8-KAlSi3O8-SiO2 H2O. Geol Soc Am Mem 74

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Anderson, J.R. Petrology of a portion of the Eastern Peninsular Ranges mylonite zone, Southern California. Contr. Mineral. and Petrol. 84, 253–271 (1983). https://doi.org/10.1007/BF00371290

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00371290

Keywords

Navigation