1995
DOI: 10.1080/00206819509465420
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Petrotectonic Evolution of the Maksyutov Complex, Southern Urals, Russia: Implications for Ultrahigh-Pressure Metamorphism

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Cited by 70 publications
(47 citation statements)
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“…Most studies of the Maksyutov Complex have concentrated on three key localities ± Karayanovo, Shubino and Antingan (Figure 1) ± where ma®c eclogites and blueschists occur as layers and boudins in metasedimentary rocks of the lower unit 1. The presence of jadeite, glaucophane, phengite and garnet in the metasediments demonstrates that they experienced similar pressure±temperature (P±T) conditions as the ma®c eclogites and blueschists Lennykh et al 1995;Dobretsov et al 1996;Hetzel et al 1998).…”
Section: P±t Evolutionmentioning
confidence: 96%
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“…Most studies of the Maksyutov Complex have concentrated on three key localities ± Karayanovo, Shubino and Antingan (Figure 1) ± where ma®c eclogites and blueschists occur as layers and boudins in metasedimentary rocks of the lower unit 1. The presence of jadeite, glaucophane, phengite and garnet in the metasediments demonstrates that they experienced similar pressure±temperature (P±T) conditions as the ma®c eclogites and blueschists Lennykh et al 1995;Dobretsov et al 1996;Hetzel et al 1998).…”
Section: P±t Evolutionmentioning
confidence: 96%
“…Recently, there has been some speculation about the former presence of coesite and even diamond in the Maksyutov Complex which would indicate ultrahigh-pressure metamorphic conditions Lennykh et al 1995;Leech and Ernst 1998;Leech and Stockli 2000). As this topic is highly relevant for the interpretation of the published geochronological data (see below) and the geodynamic evolution of the arc±continent collision, we brie¯y summarize the arguments for and against ultrahigh-pressure metamorphism.…”
Section: P±t Evolutionmentioning
confidence: 97%
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“…There is independent geologic evidence of continental collision in the Late Precam brian, which may have resulted in eclogite formation [Gee et al, 1996;Giese et al, 1999]. In addition, there are eclogitic rocks exposed at the surface and preserved in the high-grade metamorphic Maksyutov Complex [Beane et aI., 1995;Lennykh et al, 1995Lennykh et al, , 1997Leech and Stockli, 2000]. These eclogites have been dated as Devonian in age (377-384 Ma) based on U-Pb decay ages of rutile within the mafic eclogite [Beane et aI., 1995[Beane et aI., , 1997Beane and Conelly, 2000].…”
Section: The Case For Phase-change Mohomentioning
confidence: 99%
“…Lennykh et al [1995], Hetzel et al [1998], Dobretsov et al [1996], and Beane [1997] sug gested that this complex consists of three main rock types including high-pressure eclogitc facies rocks, metasand stones (blueschist-facics), and a metamorphosed mafic ultramafic melange (grecnschist facies). The protolith and the metamorphic age of the rocks forming the Maksyutov Complex remain a subject of controversy [e.g., Zakharov and Puchkov, 1994;Hetzel, 1999;Leech and Stockli, 2000].…”
Section: Geologic Frameworkmentioning
confidence: 99%