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Of the three principal rock types (igneous, sedimentary, and metamorphic), igneous rocks can be thought of as "primary" rocks because they crystallize from a liquid. Sedimentary and metamorphic rocks, which we will study later, may be thought of as derivative rocks.
The feeder system is composed of WSW ENE-striking lens-shaped stocks of layered gabbronorite and pyroxene hornblende gabbronorite, surrounded by monzodiorite. The texture of an igneous rock fine-grained vs coarse-grained is dependent on the rate of cooling of the melt slow cooling allows large crystals to form, fast cooling yields small crystals.
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Petrological Constraints on the Recycling of Mafic Crystal Mushes and Intrusion of Braided Sills in the Torres del Paine Mafic Complex (Patagonia)
Corresponding author. Present address: School of Earth Sciences, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK. Telephone: +44 (0)117 331 5181. Fax:
+44 (0)117 925 3385 . E-mail: [email protected] Search for other works by this author on: O Müntener , O Müntener Institute of Earth Sciences, Geopolis, University of Lausanne, Lausanne, Switzerland Search for other works by this author on: L P Baumgartner , L P Baumgartner Institute of Earth Sciences, Geopolis, University of Lausanne, Lausanne, Switzerland Search for other works by this author on: B Putlitz B Putlitz Institute of Earth Sciences, Geopolis, University of Lausanne, Lausanne, Switzerland Search for other works by this author on:Journal of Petrology, Volume 55, Issue 5, May 2014, Pages 917–949, https://doi.org/10.1093/petrology/egu011
Published: 12 April 2014 Received: 23 July 2013 Accepted: 28 February 2014 Published: 12 April 2014 ViewsCite
J Leuthold, O Müntener, L P Baumgartner, B Putlitz, Petrological Constraints on the Recycling of Mafic Crystal Mushes and Intrusion of Braided Sills in the Torres del Paine Mafic Complex (Patagonia), Journal of Petrology, Volume 55, Issue 5, May 2014, Pages 917–949, https://doi.org/10.1093/petrology/egu011
Navbar Search Filter Mobile Enter search term Search Navbar Search Filter Enter search term SearchCumulate and crystal mush disruption and reactivation are difficult to recognize in coarse-grained, shallow plutonic rocks. Mafic minerals included in hornblende and zoned plagioclase provide snapshots of early crystallization and cumulate formation, but are difficult to interpret in terms of the dynamics of magma ascent and possible links between silicic and mafic rock emplacement. This study presents the field relations, the microtextures and the mineral chemistry of the Miocene mafic sill complex of the Torres del Paine intrusive complex (Patagonia, Chile) and its subvertical feeder zone. We summarize a number of observations that occur in structurally different, shallow, plutonic rocks, as follows. (1) The mafic sill complex was built up by a succession of braided sills of shoshonitic and high-K calc-alkaline porphyritic hornblende-gabbro and fine-grained monzodiorite sills. Local diapiric structures and felsic magma accumulation between sills indicate limited separation of intercumulus liquid from the mafic sills. Anhedral hornblende cores, with olivine + clinopyroxene ± plagioclase ± apatite inclusions, crystallized at temperatures >900°C and pressures of ~300 to ~400 MPa. The corresponding rims and monzodiorite matrix crystallized at T >950°C) than estimated from the composition of the granite minimum. We show that hornblende–plagioclase thermobarometry is a useful monitor for the determination of the segregation conditions of granitic magmas from gabbroic crystal mushes, and for monitoring the evolution of shallow crustal magmatic crystallization, decompression and cooling.
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