Eastern Mojave Vegetation | Ronda Peridotite |
| Tom Schweich |
Topics in this Article: Literature Cited | (No Preface)
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The Ronda massif is the largest surface exposure of peridotite on Earth. All three peridotite facies (garnet, spinel, and plagioclase) are represented within the 300 km2 outcrop.
| | Literature Cited: High-temperature emplacement of the
Los Reales peridotite nappe (Betic Cordillera, Spain). |
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Literature Cited:
Diapiric emplacement of the Ronda high-temperature ultramafic intrusion, southern Spain.
| | Literature Cited: Locations: Sierra Bermeja. Emplacement of the
Ronda peridotite, Sierra Bermeja, Spain |
| Literature Cited:
The Ronda peridotite: Garnet-, spinel-, and plagioclase-lherzolite facies and the P-T trajectories of a high-temperature mantle intrusion.
| | Literature Cited: Extensional collapse
of thickened continental lithosphere: A working hypothesis for the Alboran Sea and Gibraltar arc.
| | Literature Cited: Further Sr and Nd
isotopic results from peridotites of the Ronda Ultramafic Complex.
| | Literature Cited: Very high rates of
cooling and uplift in the Alpine belt of the Betic Cordilleras, southern Spain.
| | Literature Cited: Tectonic implications
of graphitized diamonds from the Ronda peridotite massif. |
| Literature Cited: Locations: Los Reales de Sierra Bermeja. Sierra Bermeja. Uplift and
emplacement of upper mantle rocks in the western Mediterranean |
| Literature Cited: Structural petrology
of the Ronda peridotite. | | Literature Cited: Origin of the
recrystallisation front in the Ronda peridotite by km-pervasive porous melt flow.
| | Literature Cited: Comment and Reply on
"Very high rates of cooling and uplift in the Alpine belt of the Betic Cordilleras, southern Spain".
| | Literature Cited: Alternating
contractional and extensional events in the Alpujarride nappes of the Alboran domain.
| | Literature Cited: Sequential
development of the metamorphic aureole beneath the Ronda peridotites and it bearing on the tectonic evolution of the Betic Cordillera
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Literature Cited: Locations: Carratraca Massif.
Attenuation and excision of a crustal section during extensional exhumation: The Carratraca massif, southern Spain.
| | Literature Cited: Active continental
subduction beneath the Betic Cordillera and the Alboran Sea. |
| Literature Cited: Mesozoic formation of
pyroxenites and gabbros in the Ronda area (southern Spain), followed by early Miocene subduction metamorphism and emplacement into the middle crust: U-Pb sensitive high-resolution ion microprobe dating of zircon.
| | Literature Cited: Xonotlite in
rodingite assemblages from the Ronda peridotites, Betic Cordilleras, southern Spain.
| | Literature Cited: Locations: Sierra de Aguas. Sierra de la Robla. Tubia et al., examined the
foliations of the Carratraca massif (Sierra de Aguas and Sierra de la Robla) that supports the injection of hot asthenosphere into older into older and cooler lithospheric mantle during the emplacement of the Ronda Peridotite.
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| Literature CitedA list of all literature cited by this web site can be found in the Bibliography.
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| Argles, T. W., J. P. Platt, and D. J. Waters. 1999. Attenuation and excision of a crustal section during extensional exhumation" The Carratraca massif, southern Spain. Geological Society [London] Journal. 156: 149-162. {TAS-pdf} Location records referred to by this literature:
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| Balanyá, J. C., V. Garciá-Dueñas, and J. M. Azañón. 1997. Alternating contractional and extensional events in the Alpujarride nappes of the Alboran domain (Betics, Gibraltar Arc). Tectonics. 16: 226-238.
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| Davies, G. R., P. H. Nixon, D. G. Pearson, and M. Obata. 1993. Tectonic implications of graphitized diamonds from the Ronda peridotite massif, southern Spain. Geology. 21: 471-474. {TAS-pdf}
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| de Jong, Koen, H. P. Zeck, P. Monié and I. M. Villa. 1992. Comment and Reply on "Very high rates of cooling and uplift in the Alpine belt of the Betic Cordilleras, southern Spain". Geology. 20: 1052-1054.
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| Esteban, J. J., J. Cuevas, J. M. Tubía, and I. Yusta. 2003. Xonotlite in rodingite assemblages from the Ronda peridotites, Betic Cordilleras, southern Spain. Canadian Mineralogist. 41: 161-170.
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| Loomis, T. H. 1972. Diapiric emplacement of the Ronda high-temperature ultramafic intrusion, southern Spain. GSA Bulletin. 83: 2475-2496.
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| Lundeen, M. T. 1978. Emplacement of the Ronda peridotite, Sierra Bermeja, Spain. GSA Bulletin. 89: 172-180. {TAS-pdf} Location records referred to by this literature:
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| Morales, J., I. Serrano, A. Jabaloy, J. Galindo-Zaldívar, D. Zhao, F. Torcal, F. Vidal, and F. González-Lodeiro. 1999. Active continental subduction beneath the Betic Cordillera and the Alboran Sea. Geology. 27: 735-738. {TAS-pdf}
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| Obata, M. 1980. The Ronda peridotite: Garnet-, spinel-, and plagioclase-lherzolite facies and the P-T trajectories of a high-temperature mantle intrusion. Journal of Petrology. 21: 533-572.
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| Platt, J. P., and R. L. M. Vissers. 1989. Extensional collapse of thickened continental lithosphere: A working hypothesis for the Alboran Sea and Gibraltar arc. Geology. 17: 540-543. {TAS-pdf}
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| Reisberg, L., A. Zindler, and E. Jagoutz. 1989. Further Sr and Nd isotopic results from peridotites of the Ronda Ultramafic Complex. Earth and Planetary Science Letters. 96: 161-180. |
| Sánchez-Rodríguez, L., and D. Gebauer. 2000. Mesozoic formation of pyroxenites and gabbros in the Ronda area (southern Spain), followed by early Miocene subduction metamorphism and emplacement into the middle crust: U-Pb sensitive high-resolution ion microprobe dating of zircon. Tectonophysics. 316: 19-44.
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| Tubía, J. M. and J. Cuevas. 1986. High-temperature emplacement of the Los Reales peridotite nappe (Betic Cordillera, Spain). Journal of Structural Geology. 8: 473-482.
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| Tubía, J. M., J. Cuevas, and J. J. Esteban. 2004. Tectonic evidence in the Ronda peridotites, Spain, for mantle diapirism related to delamination. Geology. 32(11):941-944. {TAS-pdf} Location records referred to by this literature:
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| Tubía, J. M., J. Cuevas, and J. I. Gil Ibarguchi. 1997. Sequential development of the metamorphic aureole beneath the Ronda peridotites and it bearing on the tectonic evolution of the Betic Cordillera. Tectonophysics. 279: 227-252.
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| Van der Wal, Dirk, and Reinoud L. M. Vissers. 1993. Uplift and emplacement of upper mantle rocks in the western Mediterranean. Geology. 21: 1119-1122. {TAS-pdf} Location records referred to by this literature:
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| Van der Wal, D., and R. L. M. Vissers. 1996. Structural petrology of the Ronda peridotite. Journal of Petrology. 37: 23-43.
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| Van del Wal, D., and J. L. Bodinier. 1996. Origin of the recrystallisation front in the Ronda peridotite by km-pervasive porous melt flow. Contributions to Mineralogy and Petrology. 122: 387-405.
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| Zeck, H. P., P. Monié, I. M. Villa and B. T. Hansen. 1992. Very high rates of cooling and uplift in the Alpine belt of the Betic Cordilleras, southern Spain. Geology. 20: 79-82. {TAS-pdf} If you have a question or a comment
you may write to me at: tas4@schweich.com I sometimes post
interesting questions in my FAQ, but I never disclose your full name or address.
| | Date and time this article was prepared: 6/30/2008 10:49:13 AM |