Abstract
The Magma Chamber Simulator (MCS) is a thermodynamic tool for modeling the evolution of magmatic systems that are open with respect to assimilation of partial melts or stoped blocks, magma recharge + mixing, and fractional crystallization. MCS is available for both PC and Mac. In the MCS, the thermal, mass, and compositional evolution of a multicomponent–multiphase composite system of resident magma, wallrock, and recharge reservoirs is tracked by rigorous self-consistent thermodynamic modeling. A Recharge–Assimilation (Assimilated partial melt or Stoped blocks)–Fractional Crystallization (RnASnFC; ntot ≤ 30) scenario is computed by minimization or maximization of appropriate thermodynamic potentials using the family of rhyolite- and pMELTS engines coupled to an Excel Visual Basic interface. In MCS, during isobaric cooling and crystallization, resident magma thermally interacts with wallrock that is in internal thermodynamic equilibrium. Wallrock partial melt above a user-defined percolation threshold is homogenized (i.e., brought in to chemical potential equilibrium) with resident magma. Crystals that form become part of a cumulate reservoir that remains thermally connected but chemically isolated from resident melt. Up to 30 instances (n ≤ 30) of magma mixing by recharge and/or bulk assimilation of stoped wallrock blocks can occur in a single simulation; each recharge magma or stoped block has a unique user-defined composition and thermal state. Recharge magmas and stoped blocks hybridize (equilibrate) with resident melt, yielding a single new melt composition and temperature. MCS output includes major and trace element concentrations and isotopic ratios (Sr, Nd, Hf, Pb, Os, and O as defaults) of wallrock, recharge magma/stoped blocks, resident magma melt, and cumulates. The chemical formulae of equilibrium crystalline phases in the cumulate reservoir, wallrock, and recharge magmas/stoped blocks are also output. Depending on the selected rhyolite-MELTS engine, the composition and properties of a possible supercritical fluid phase (H2O and/or CO2) are also tracked. Forward modeling of theoretical magma systems and suites of igneous rocks provides quantitative insight into key questions in igneous petrology such as mantle versus crustal contributions to terrestrial magmas, the record of magmatism preserved in cumulates and exsolved fluids, and the chronology of RASFC processes that may be recorded by crystal populations, melt inclusions, and whole rocks. Here, we describe the design of the MCS software that focuses on major element compositions and phase equilibria (MCS-PhaseEQ). Case studies that involve fractional crystallization, magma recharge + mixing, and crustal contamination of a depleted basalt that resides in average upper crust illustrate the major element and phase equilibria consequences of these processes and highlight the rich array of data produced by MCS. The cases presented here, which represent an infinitesimal fraction of possible RASFC processes and bulk compositions, show that the records of recharge and/or crustal contamination may be subtle and are not necessarily those that would be predicted using conventional intuition and simple mass balance arguments. Mass and energy constrained thermodynamic tools like the MCS quantify the open-system evolution of magmas and provide a systematic understanding of the petrology and geochemistry of open system magmatic processes. The trace element and isotope MCS computational tool (MCS-Traces) is described in a separate contribution (part II).
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References
Albarède F (1995) Introduction to geochemical modeling. Cambridge University Press, Cambridge
Ambler EP, Ashley PM (1977) Vermicular orthopyroxene-magnetite symplectites from the Wateranga layered mafic intrusion, Queensland, Australia. Lithos 10:163–172. https://doi.org/10.1016/0024-4937(77)90044-5
Arndt NT, Czamanske GK, Wooden JL, Fedorenko VA (1993) Mantle and crustal contributions to continental flood volcanism. Tectonophysics 223:39–52. https://doi.org/10.1016/0040-1951(93)90156-e
Asimow PD, Ghiorso MS (1998) Algorithmic modifications extending MELTS to calculate subsolidus phase relations. Am Miner 83:1127–1131
Asmerom Y, Patchett PJ, Damon PE (1991) Crust-mantle interaction in continental arcs: inferences from the Mesozoic arc in the southwestern United States. Contrib Mineral Petrol 107:124–134. https://doi.org/10.1007/BF00311190
Baker JA, Macpherson CG, Menzies MA, Thirlwall MF, AL-Kadasi M, Mattey DP (2000) Resolving crustal and mantle contributions to continental flood volcanism, Yemen; constraints from mineral oxygen isotope data. J Petrol 41:1805–1820. https://doi.org/10.1093/petrology/41.12.1805
Becerril L, Galindo I, Gudmundsson A, Morales JM (2013) Depth of origin of magma in eruptions. Sci Rep 3:2762. https://doi.org/10.1038/srep02762
Bohrson WA, Spera FJ, Ghiorso MS, Brown GA, Creamer JB, Mayfield A (2014) Thermodynamic model for energy-constrained open-system evolution of crustal magma bodies undergoing simultaneous recharge, assimilation and crystallization: the magma chamber simulator. J Petrol 55:1685–1717. https://doi.org/10.1093/petrology/egu036
Borisova AY, Bohrson WA, Grégoire M (2017) Origin of primitive ocean island basalts by crustal gabbro assimilation and multiple recharge of plume-derived melts. Geochem Geophys Geosyst 18:2701–2716. https://doi.org/10.1002/2017GC006986
Bowen NL (1928) The evolution of igneous rocks. Dover Publications, New York, p 334
Coogan LA, Saunders AD, Wilson RN (2014) Aluminum-in-olivine thermometry of primitive basalts: evidence of an anomalously hot mantle source for large igneous provinces. Chem Geol 368:1–10. https://doi.org/10.1016/j.chemgeo.2014.01.004
Costa F, Dohmen R, Chakraborty S (2008) Time scales of magmatic processes from modeling the zoning patterns of crystals. In: Putirka KD, Tepley FJ III (eds) Minerals, inclusions and volcanic processes, vol 69. Mineralogical Society of America, Chantilly, pp 545–594. https://doi.org/10.2138/rmg.2008.69.14
Couch S, Sparks RSJ, Carroll MR (2001) Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers. Nature 411:1037–1039. https://doi.org/10.1038/35082540
Cox KG, Hawkesworth CJ (1984) Relative contribution of crust and mantle to flood basalt magmatism, Mahabaleshwar area, Deccan Traps. Philos Trans Royal Soc London Ser A, Math Phys Sci 310:627–641. https://doi.org/10.1098/rsta.1984.0011
Davidson JP, Tepley FJ (1997) Recharge in volcanic systems: evidence from isotope profiles of phenocrysts. Science 80(275):826–829. https://doi.org/10.1126/science.275.5301.826
Davidson JP, Morgan DJ, Charlier BLA, Harlou R, Hora JM (2007) Microsampling and isotopic analysis of igneous rocks: implications for the study of magmatic systems. Ann Rev Earth Planet Sci 35:273–311
DePaolo DJ (1981) Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization. Earth Planet Sci Lett 53:189–202. https://doi.org/10.1016/0012-821x(81)90153-9
Edwards MA, Jackson MG, Kylander-Clark ARC, Harvey J, Hagen-Peter GA, Seward GGE, Till CB, Adams JV, Cottle JM, Hacker BR, Spera FJ (2019) Extreme enriched and heterogenous 87Sr/86Sr ratios recorded in magmatic plagioclase from the Samoan hotspot. Earth Planet Sci Lett 511:190–201. https://doi.org/10.1016/j.epsl.2019.01.040
Erdmann S, Scaillet B, Kellett DA (2012) Textures of peritectic crystals as guides to reactive minerals in magmatic systems: new insights from melting experiments. J Petrol 53:2231–2258. https://doi.org/10.1093/petrology/egs048
Fries C (1939) Resorbed feldspar in a basalt flow. Am Mineral 24(12):782–790
Ghiorso MS, Sack RO (1995) Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contrib Mineral Petrol 119:197–212. https://doi.org/10.1007/bf00307281
Ghiorso MS, Gualda GAR (2015) An H2O–CO2 mixed fluid saturation model compatible with rhyolite-MELTS. Contrib Mineral Petrol 169:53. https://doi.org/10.1007/s00410-015-1141-8
Ghiorso MS, Hirschmann MM, Reiners PW, Kress VC III (2002) The pMELTS: a revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa. Geochem Geophys Geosyst 3:1–35. https://doi.org/10.1029/2001GC000217
Ginibre C, Wörner G, Kronz A (2007) Crystal zoning as an archive for magma evolution. Elements 3:261–266. https://doi.org/10.2113/gselements.3.4.261
Grove TL, Kinzler RJ, Bryan WB (1992) Fractionation of mid-ocean ridge basalt (MORB). In: Morgan JP, Blackman DK, Sinton JM (eds) Mantle flow and melt generation at mid-ocean ridges, geophysical monograph series. Geophysical monograph series, vol 71. American Geophysical Union, Washington, pp 281–310. https://doi.org/10.1029/GM071p0281
Gualda GAR, Ghiorso MS, Lemons RV, Carley TL (2012) Rhyolite-MELTS: a modified calibration of MELTS optimized for Silica-rich, fluid-bearing magmatic systems. J Petrol 53:875–890. https://doi.org/10.1093/petrology/egr080
Heinonen JS, Luttinen AV, Spera FJ, Bohrson WA (2019) Deep open storage and shallow closed transport system for a continental flood basalt sequence revealed with Magma Chamber Simulator. Contrib Mineral Petrol 174(11):87
Heinonen JS, Bohrson WA, Spera FJ, Brown GA, Scruggs M, Adams J (2020) Diagnosing open-system magmatic processes using the Magma Chamber Simulator (MCS): part II—trace elements and isotopes. Contrib Mineral Petrol. https://doi.org/10.1007/s00410-020-01718-9
Hildreth W, Moorbath S (1988) Crustal contributions to arc magmatism in the Andes of Central Chile. Contrib Mineral Petrol 98:455–489. https://doi.org/10.1007/BF00372365
Lesher CE, Spera FJ (2015) Thermodynamic and transport properties of silicate melts and magma. In: Sigurdsson H (ed) The encyclopedia of volcanoes, 2nd edn. Academic Press, Amsterdam, pp 113–141. https://doi.org/10.1016/b978-0-12-385938-9.00005-5
Luttinen AV, Furnes H (2000) Flood basalts of Vestfjella: Jurassic magmatism across an Archaean-Proterozoic lithospheric boundary in Dronning Maud Land, Antarctica. J Petrol 41:1271–1305. https://doi.org/10.1093/petrology/41.8.1271
Mangiacapra A, Moretti R, Rutherford M, Civetta L, Orsi G, Papale P (2008) The deep magmatic system of the Campi Flegrei caldera (Italy). Geophys Res Lett. https://doi.org/10.1029/2008GL035550
Moore NE, Grunder AL, Bohrson WA (2018) The three-stage petrochemical evolution of the Steens Basalt (southeast Oregon, USA) compared to large igneous provinces and layered mafic intrusions. Geosphere 14:2505–2532. https://doi.org/10.1130/GES01665.1
Neave DA, Putirka KD (2017) A new clinopyroxene-liquid barometer, and implications for magma storage pressures under Icelandic rift zones. Am Min 102:777–794. https://doi.org/10.2138/am-2017-5968
Oldenburg CM, Spera FJ, Yuen DA, Sewell G (1989) Dynamic mixing in magma bodies: theory, simulations, and implications. J Geophys Res 94:9215–9236. https://doi.org/10.1029/JB094iB07p09215
Powell R, Holland TJB (1988) An internally consistent dataset with uncertainties and correlations: 3. Applications to geobarometry, worked examples and a computer program. J Metamorph Petrol. https://doi.org/10.1111/j.1525-1314.1988.tb00415.x
Powell R, Holland TJB (1994) Optimal geothermometry and geobarometry. Am Mineral 79:120–133
Powell R, Holland TJB, Worley B (1998) Calculating phase diagrams involving solid solution via non-linear equations, with examples from THERMOCALC. J Metamorph Petrol. https://doi.org/10.1111/j.1525-1314.1998.00157.x
Putirka KD (2008) Excess temperatures at ocean islands: implications for mantle layering and convection. Geology (Boulder) 36:283–286. https://doi.org/10.1130/G24615A.1
Putirka K (2017) Geothermometry and geobarometry. In: White WM (ed) Encyclopedia of geochemistry: a comprehensive reference source on the chemistry of the Earth. Springer International Publishing, Cham, pp 1–19. https://doi.org/10.1007/978-3-319-39193-9_322-1
Rudnick RL, Gao S (2003) The composition of the continental crust. In: Rudnick RL (ed) The crust, treatise on geochemistry, vol 3. Elsevier-Pergamon, Oxford, pp 1–64. https://doi.org/10.1016/b0-08-043751-6/03016-4
Scruggs MA, Putirka KD (2018) Eruption triggering by partial crystallization of mafic enclaves at Chaos Crags, Lassen Volcanic Center, California. Am Min 103:1575–1590
Spera FJ, Bohrson WA (2001) Energy-constrained open-system magmatic processes I: general model and energy-constrained assimilation and fractional crystallization (EC-AFC) formulation. J Petrol 42:999–1018. https://doi.org/10.1093/petrology/42.5.999
Spera FJ, Schmidt JS, Bohrson WA, Brown GA (2016) Dynamics and thermodynamics of magma mixing: Insights from a simple exploratory model. Am Min 101:627–643. https://doi.org/10.2138/am-2016-5305
Stern R, Johnson PR (2010) Continental lithosphere of the Arabian Plate: a geologic, petrologic, and geophysical synthesis. Earth-Sci Rev. https://doi.org/10.1016/j.earscirev.2010.01.002
Streck MJ (2008) Mineral textures and zoning as evidence for open system processes. Rev Mineral Geochem 69:595–622. https://doi.org/10.2138/rmg.2008.69.15
Takach MK (2018) Quantifying crustal assimilation in historical to recent (1329–2005) Lavas at Mt. Etna, Italy: Insights from Thermodynamic Modeling. Thesis, Central Washington University. https://digitalcommons.cwu.edu/etd/1006
Taylor HP Jr (1980) The effects of assimilation of country rocks by magmas of 18O/16O and 87Sr/86Sr in igneous rocks. Earth Planet Sci Lett. https://doi.org/10.1016/0012-821X(80)90040-0
Tepley FJ III, Davidson JP, Tilling RI, Arth JG (2000) Magma mixing, recharge and eruption histories recorded in plagioclase phenocrysts from El Chichón Volcano, Mexico. J Petrol 41:1397–1411. https://doi.org/10.1093/petrology/41.9.1397
Tepley FJ III, de Silva S, Salas G (2013) Magma Dynamics and Petrological Evolution Leading to the VEI 5 2000 BP Eruption of El Misti Volcano Southern Peru. J Petrol 54(10):2033–2065. https://doi.org/10.1093/petrology/egt040
Tikoff B, Teyssier C (1992) Crustal-scale, en echelon “P-shear” tensional bridges: a possible solution to the batholithic room problem. Geology 20:927–930. https://doi.org/10.1130/0091-7613(1992)020<0927:CSEEPS>2.3.CO;2
Ubide T, Kamber BS (2018) Volcanic crystals as time capsules of eruption history. Nat Commun 9:326. https://doi.org/10.1038/s41467-017-02274-w
Ubide T, Mollo S, Zhao J, Nazzari M, Scarlato P (2019) Sector-zoned clinopyroxene as a recorder of magma history, eruption triggers, and ascent rates. Geochim Cosmochim Acta 251:265–283. https://doi.org/10.1016/j.gca.2019.02.021
Villiger S, Müntener O, Ulmer P (2007) Crystallization pressures of mid-ocean ridge basalts derived from major element variations of glasses from equilibrium and fractional crystallization experiments. J Geophys Res. https://doi.org/10.1029/2006JB004342
Wade JA, Plank T, Hauri EH, Kelley KA, Roggensack K, Zimmer M (2008) Prediction of magmatic water contents via measurement of H2O in clinopyroxene phenocrysts. Geology 36:799–802. https://doi.org/10.1130/G24964A.1
Walker JA, Williams SN, Kalamarides RI, Feigenson MD (1993) Shallow open-system evolution of basaltic magma beneath a subduction zone volcano: the Masaya Caldera Complex, Nicaragua. J Volcanol Geotherm Res 56:379–400. https://doi.org/10.1016/0377-0273(93)90004-B
Wark DA, Hildreth W, Spear FS, Cherniak DJ, Watson EB (2007) Pre-eruption recharge of the Bishop magma system. Geology 35:235–238. https://doi.org/10.1130/G23316A.1
Weber G, Castro JM (2017) Phase petrology reveals shallow magma storage prior to large explosive silicic eruptions at Hekla volcano, Iceland. Earth Planet Sci Lett 466:168–180. https://doi.org/10.1016/j.epsl.2017.03.015
Wiebe RA (1968) Plagioclase stratigraphy; a record of magmatic conditions and events in a granite stock. Am J Sci 266:690–703. https://doi.org/10.2475/ajs.266.8.690
Wooden JL, Czamanske GK, Fedorenko VA, Arndt NT, Chauvel C, Bouse RM, King BW, Knight RJ, Siems DF (1993) Isotopic and trace-element constraints on mantle and crustal contributions to Siberian continental flood basalts, Noril’sk area, Siberia. Geochim Cosmochim Acta 57:3677–3704
Yoder HS, Tilley CE (1962) Origin of basalt magmas: an experimental study of natural and synthetic rock systems. J Petrol 3:342–532. https://doi.org/10.1093/petrology/3.3.342
Acknowledgements
We are indebted to numerous MCS users and workshop attendees who have contributed to improving MCS. We also thank CWU students Jennifer McLeod, Alec Melone, Rachel Sanchez, and Rebekah Krohn for their work on improving MCS. We also send a hearty thank you to Dr. Mark Ghiorso, whose cooperation in developing MCS, was critical. We thank an anonymous reviewer and Paul Asimow for insightful reviews and Othmar Muntener for his expert editorial handling. This work was funded by NSF Grants to WA Bohrson and FJ Spera and by the Academy of Finland Grants 295129 and 306962 to JS Heinonen and E Suikkanen.
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Bohrson, W.A., Spera, F.J., Heinonen, J.S. et al. Diagnosing open-system magmatic processes using the Magma Chamber Simulator (MCS): part I—major elements and phase equilibria. Contrib Mineral Petrol 175, 104 (2020). https://doi.org/10.1007/s00410-020-01722-z
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DOI: https://doi.org/10.1007/s00410-020-01722-z