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Artículos de revistas sobre el tema "Petrogenesis"

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Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 30 de julio de 2024

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1

Janoušek, Vojtěch y Jean-François Moyen. "Whole-rock geochemical modelling of granite genesis: the current state of play". Geological Society, London, Special Publications 491, n.º 1 (6 de febrero de 2019): 267–91. http://dx.doi.org/10.1144/sp491-2018-160.

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AbstractWhole-rock geochemistry represents a powerful tool in deciphering petrogenesis of magmatic suites, including granitoids, which can be used to formulate and test hypotheses qualitatively and often also quantitatively. Typically, it can rule out impossible/improbable scenarios and further constrain the process inferred on geological and petrological grounds. With the current explosion of high-precision data, both newly acquired and retrieved from extensive databases, the whole-rock geochemistry-based petrogenetic modelling of igneous rocks will gain further importance. Especially promising is its combination with thermodynamic modelling into a single, coherent and comprehensive software, using the R and Python languages.

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2

Leeman, William P. "Igneous petrogenesis". Geochimica et Cosmochimica Acta 61, n.º 10 (mayo de 1997): 2147. http://dx.doi.org/10.1016/s0016-7037(97)83223-1.

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3

Castillo, Paterno R. "Adakite petrogenesis". Lithos 134-135 (marzo de 2012): 304–16. http://dx.doi.org/10.1016/j.lithos.2011.09.013.

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4

Grove, T. L. y R. J. Kinzler. "Petrogenesis of Andesites". Annual Review of Earth and Planetary Sciences 14, n.º 1 (mayo de 1986): 417–54. http://dx.doi.org/10.1146/annurev.ea.14.050186.002221.

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5

Floss, Christine, Ghislaine Crozaz, Gordon McKay, Takashi Mikouchi y Marvin Killgore. "Petrogenesis of angrites". Geochimica et Cosmochimica Acta 67, n.º 24 (diciembre de 2003): 4775–89. http://dx.doi.org/10.1016/s0016-7037(03)00310-7.

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6

Canil, Dante. "The geochemistry of komatiites and basalts from the Deadman Hill area, Munro Township, Ontario, Canada". Canadian Journal of Earth Sciences 24, n.º 5 (1 de mayo de 1987): 998–1008. http://dx.doi.org/10.1139/e87-097.

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A sequence of Archean komatiites (> 18 wt.% MgO), komatiitic basalts (10–18 wt.% MgO), high-Mg tholeiites (6–10 wt.% MgO), and high-Fe tholeiites (< 8 wt.% MgO) is exposed in the Deadman Hill area of Munro Township, Ontario, Canada. Major- and trace-element analyses of 28 samples are used to assess their petrogenetic significance. The use of molecular proportion ratio plots shows the samples have maintained their primary SiO2, FeO*, MgO, TiO2, Al2O3, Ni, Cr, Zr, Y, and V contents. Secondary redistribution of Na2O, K2O, Rb, Sr, Ba, and, in some samples, CaO has occurred.Covariation in both major- and trace-element data suggests the komatiites are primary melts that equilibrated with a harzburgite residua at pressures of 3–6 GPa. Garnet did not have a major role in their petrogenesis or in the petrogenesis of spatially related komatiitic basalts and high-Mg tholeiites. Major- and trace-element variation in komatiitic basalts with 17–12 wt.% MgO requires that they be partial melts in equilibrium with clinopyroxene at pressures of < 3 GPa. They are unrelated to the komatiites. Both lower degree partial melting of the same source as lavas with 17–12 wt.% MgO and crystal fractionation of clinopyroxene from liquids with ~12 wt.% MgO can model the evolution of less magnesian komatiitic basalts and high-Mg tholeiites. The Zr/Y and Zr/Ti ratios of the high-Fe tholeiites indicate that they are unrelated to the komatiites, komatiitic basalts, and high-Mg tholeiites and were derived by partial melting of a garnet lherzolite source.

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7

Carnevale, Gabriele, Antonio Caracausi, Alessandra Correale, Laura Italiano y Silvio G. Rotolo. "An Overview of the Geochemical Characteristics of Oceanic Carbonatites: New Insights from Fuerteventura Carbonatites (Canary Islands)". Minerals 11, n.º 2 (15 de febrero de 2021): 203. http://dx.doi.org/10.3390/min11020203.

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The occurrence of carbonatites in oceanic settings is very rare if compared with their continental counterpart, having been reported only in Cape Verde and Canary Islands. This paper provides an overview of the main geochemical characteristics of oceanic carbonatites, around which many debates still exist regarding their petrogenesis. We present new data on trace elements in minerals and whole-rock, together with the first noble gases isotopic study (He, Ne, Ar) in apatite, calcite, and clinopyroxene from Fuerteventura carbonatites (Canary Islands). Trace elements show a similar trend as Cape Verde carbonatites, almost tracing the same patterns on multi-element and REE abundance diagrams. 3He/4He isotopic ratios of Fuerteventura carbonatites reflect a shallow (sub-continental lithospheric mantle, SCLM) He signature in their petrogenesis, and they clearly differ from Cape Verde carbonatites, i.e., fluids from a deep and low degassed mantle with a primitive plume-derived He signature are involved in their petrogenesis.

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8

Hess, Paul C. "Petrogenesis of lunar troctolites". Journal of Geophysical Research 99, E9 (1994): 19083. http://dx.doi.org/10.1029/94je01868.

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9

Roberts, Stephen y Christopher Neary. "Petrogenesis of ophiolitic chromitite". Geological Society, London, Special Publications 76, n.º 1 (1993): 257–72. http://dx.doi.org/10.1144/gsl.sp.1993.076.01.12.

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10

McGregor, V. R. "Igneous Petrogenesis. Marjorie Wilson". Journal of Geology 98, n.º 5 (septiembre de 1990): 799. http://dx.doi.org/10.1086/629451.

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11

O’HARA, M. J. "Flood Basalts and Lunar Petrogenesis". Journal of Petrology 41, n.º 7 (1 de julio de 2000): 1121–25. http://dx.doi.org/10.1093/petrology/41.7.1121.

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12

Singletary, Steven y Timothy L. Grove. "Experimental constraints on ureilite petrogenesis". Geochimica et Cosmochimica Acta 70, n.º 5 (marzo de 2006): 1291–308. http://dx.doi.org/10.1016/j.gca.2005.10.034.

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13

Ringwood, A. E. "Mantle dynamics and basalt petrogenesis". Tectonophysics 112, n.º 1-4 (marzo de 1985): 17–34. http://dx.doi.org/10.1016/0040-1951(85)90170-2.

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14

Castillo, Paterno R. "An overview of adakite petrogenesis". Chinese Science Bulletin 51, n.º 3 (febrero de 2006): 257–68. http://dx.doi.org/10.1007/s11434-006-0257-7.

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15

Sautter, Violaine, Jean Pierre Lorand, Patrick Cordier, Benjamin Rondeau, Hugues Leroux, Cristiano Ferraris y Sylvain Pont. "Petrogenesis of mineral micro-inclusions in an uncommon carbonado". European Journal of Mineralogy 23, n.º 5 (1 de diciembre de 2011): 721–29. http://dx.doi.org/10.1127/0935-1221/2011/0023-2154.

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16

Janoušek, Vojtěch, Tomáš Navrátil, Jakub Trubač, Ladislav Strnad, František Laufek y Luděk Minařík. "Distribution of elements among minerals of a single (muscovite-) biotite granite sample – an optimal approach and general implications". Geologica Carpathica 65, n.º 4 (1 de agosto de 2014): 257–72. http://dx.doi.org/10.2478/geoca-2014-0017.

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Abstract The petrography and mineral chemistry of the coarse-grained, weakly porphyritic (muscovite-) biotite Říčany granite (Variscan Central Bohemian Plutonic Complex, Bohemian Massif) were studied in order to assess the distribution of major and trace elements among its minerals, with consequences for granite petrogenesis and availability of geochemical species during supergene processes. It is demonstrated that chemistry-based approaches are the best suited for modal analyses of granites, especially methods taking into account compositions of whole-rock samples as well as their mineral constituents, such as constrained least-squares algorithm. They smooth out any local variations (mineral zoning, presence of phenocrysts, schlieren…) and are robust in respect to the presence of phenocrysts or fabrics. The study confirms the notion that the accessory phases play a key role in incorporation of many elements during crystallization of granitic magmas. Especially the REE seem of little value in petrogenetic modelling, unless the role of accessories is properly assessed and saturation models for apatite, zircon, monazite±rutile carefully considered. At the same time, the presence of several P-, Zr- and LREE-bearing phases may have some important consequences for saturation thermometry of apatite, zircon and monazite.

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17

Cao, Ting, Qi He y ZhuQing Xue. "Petrogenesis of basaltic shergottite NWA 8656". Earth and Planetary Physics 2, n.º 5 (2018): 384–97. http://dx.doi.org/10.26464/epp2018036.

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18

O’Driscoll, Brian y José María González-Jiménez. "Petrogenesis of the Platinum-Group Minerals". Reviews in Mineralogy and Geochemistry 81, n.º 1 (14 de diciembre de 2015): 489–578. http://dx.doi.org/10.2138/rmg.2016.81.09.

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19

Nabelek, Peter I. "Petrogenesis of leucogranites in collisional orogens". Geological Society, London, Special Publications 491, n.º 1 (3 de mayo de 2019): 179–207. http://dx.doi.org/10.1144/sp491-2018-181.

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AbstractLeucogranites are a characteristic feature of collisional orogens. Their generation is intimately related to crustal thickening and the active deformation and metamorphism of metapelites. Data from Proterozoic to present day orogenic belts show that collisional leucogranites (CLGs) are peraluminous, with muscovite, biotite and tourmaline as characteristic minerals. Isotopic ratios uniquely identify the metapelitic sequences in which CLGs occur as sources. Organic material in pelitic sources results in fO2 in CLGs that is usually below the fayalite–magnetite–quartz buffer. Most CLGs form under vapour-poor conditions with melting involving a peritectic breakdown of muscovite. The low concentrations of Mg, Fe and Ti that characterize CLGs are largely related to biotite–melt equilibria in the source rocks. Concentrations of Zr, Th and rare earth elements are lower than expected from zircon and monazite saturation models because these minerals often remain enclosed in residual biotite during melting. Melting involving muscovite may limit the temperatures achieved in the source regions. A lack of nearby mantle heat sources in thick collisional orogens has led to thermal models for the generation of CLGs that involve flux melting, or large amounts of radiogenic heat generation, or decompression melting or shear heating, the last one emphasizing the link of leucogranites and their sources to crustal-scale shear zone systems.

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20

Goodenough, K. M., I. M. Coulson y F. Wall. "Intraplate alkaline magmatism: mineralogy and petrogenesis". Mineralogical Magazine 67, n.º 5 (octubre de 2003): 829–30. http://dx.doi.org/10.1180/0670829.

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21

Cronberger, Karl y Clive R. Neal. "KREEP basalt petrogenesis: Insights from 15434,181". Meteoritics & Planetary Science 52, n.º 5 (28 de febrero de 2017): 827–41. http://dx.doi.org/10.1111/maps.12837.

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22

Sossi, Paolo A., Stephen M. Eggins, Robert W. Nesbitt, Oliver Nebel, Janet M. Hergt, Ian H. Campbell, Hugh St C. O’Neill, Martin Van Kranendonk y D. Rhodri Davies. "Petrogenesis and Geochemistry of Archean Komatiites". Journal of Petrology 57, n.º 1 (enero de 2016): 147–84. http://dx.doi.org/10.1093/petrology/egw004.

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23

Anand, Mahesh, Lawrence A. Taylor, Clive R. Neal, Gregory A. Snyder, Allan Patchen, Yuji Sano y Kentaro Terada. "Petrogenesis of lunar meteorite EET 96008". Geochimica et Cosmochimica Acta 67, n.º 18 (septiembre de 2003): 3499–518. http://dx.doi.org/10.1016/s0016-7037(03)00134-0.

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24

Longhi, John. "Phase equilibrium constraints on angrite petrogenesis". Geochimica et Cosmochimica Acta 63, n.º 3-4 (febrero de 1999): 573–85. http://dx.doi.org/10.1016/s0016-7037(98)00280-4.

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25

Aertgeerts, Geoffrey, Jean Pierre Lorand, Christophe Monnier y Carole La. "Petrogenesis of South Armorican serpentinized peridotites". Lithos 314-315 (agosto de 2018): 100–118. http://dx.doi.org/10.1016/j.lithos.2018.05.013.

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26

Wyllie, Peter J. "Experimental petrology: Quantitative boundaries for petrogenesis". Journal of Earth System Science 99, n.º 1 (marzo de 1990): 5–19. http://dx.doi.org/10.1007/bf02871892.

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27

Hutton, D. H. W. y R. J. Reavy. "Strike-slip tectonics and granite petrogenesis". Tectonics 11, n.º 5 (octubre de 1992): 960–67. http://dx.doi.org/10.1029/92tc00336.

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28

Sotiriou, Paul y Ali Polat. "Petrogenesis of anorthosites throughout Earth history". Precambrian Research 384 (enero de 2023): 106936. http://dx.doi.org/10.1016/j.precamres.2022.106936.

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29

Jambon, A., V. Sautter, J. A. Barrat, J. Gattacceca, P. Rochette, O. Boudouma, D. Badia y B. Devouard. "Northwest Africa 5790: Revisiting nakhlite petrogenesis". Geochimica et Cosmochimica Acta 190 (octubre de 2016): 191–212. http://dx.doi.org/10.1016/j.gca.2016.06.032.

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30

Mishra, V. K., R. N. Tiwari, C. B. Verma, A. Mukherjee, R. K. Dixit y G. Prabhakar. "Kimberlitic olivine – a proxy to kimberlite petrogenesis and ascent process". IOP Conference Series: Earth and Environmental Science 1032, n.º 1 (1 de junio de 2022): 012027. http://dx.doi.org/10.1088/1755-1315/1032/1/012027.

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Abstract In kimberlite, olivine is an important constituent and it is found as mineral grains of different sizes, which can be of xenocrystic and magmatic origin. To know the processes, that are involved and controls the compositional variations of olivine, can provide distinct understanding into the genesis and evolution of kimberlites. In addition to this the textural features of kimberlitic olivine, which are recorded as textural events during magma assent constrains the ascent of kimberlite and the processes involved. Unambiguous identification of kimberlitic olivine and its textural features require careful petrographic examination combined with mineral compositional analysis and use of high magnification images (BSE-SEM), all this is integrated to know the origin of olivine grain which in turn constrain the process involved in ascent of kimberlite and its petrogenesis. In this study we review the use of kimberlitic olivine in deducing the upper mantle conditions and process for kimberlite petrogenesis.

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31

Hasria, Masri, Muhammad Arba Azzaman y Muhamad Jerniawan. "Petrogenetic Study on Ultramafic Rocks from Waturapa and Surrounding Areas, South Konawe Regency, Southeast Sulawesi Province". Journal of Geoscience, Engineering, Environment, and Technology 8, n.º 1 (27 de marzo de 2023): 10–16. http://dx.doi.org/10.25299/jgeet.2023.8.1.11035.

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The petrogenesis study of ultramafic igneous rocks in the South Konawe Region has been carried out by several previous researchers, however, petrogenesis of ultramafic igneous rocks in the Waturapa Region has never been carried out in detail. This study aims to determine the characteristics and petrogenesis of ultramafic igneous rocks in the Waturapa area using petrographic and geochemical analysis using the XRF method. Petrographic analysis was carried out to determine the relative abundance percentage of primary minerals in the form of olivine, clinopyroxene, orthopyroxene, and opaque minerals as well as secondary serpentine minerals which were formed later. Meanwhile, XRF geochemical analysis is used to determine the major and minor oxide content in rocks. This geochemical data is used to determine ultramafic rock types, and magma series and to interpret the tectonic setting of the research location. The results showed that the ultramafic rocks in the study area consisted of olivine websterite and lherzolite, both of which have been serpentinized which is characterized by the presence of serpentine minerals such as lizardite and chrysotile. These serpentine minerals are present as replacement minerals and fracture-filling minerals. The geochemical characteristics of the analyzed rocks showed a SiO2 content of less than 45%, high MgO content, and low K2O, TiO2, Na2O3, and P2O5 compounds. The igneous rocks in the study area are classified as ultrabasic or ultramafic rocks (peridot gabbro). Ultramafic rocks in the study area belong to the tholeiitic magma series that formed in oceanic islands or oceanic intraplate margins.

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32

Volker, J. A. y B. G. J. Upton. "Reply to comments by J. H. Bédard and R. S. J. Sparks". Transactions of the Royal Society of Edinburgh: Earth Sciences 82, n.º 4 (1991): 391. http://dx.doi.org/10.1017/s0263593300004235.

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Bédard and Sparks' (BS) comments are very much appreciated as they giveus the opportunity to emphasise certain aspects of our observations which, in turn, mayclarify the discussion on the petrogenesis of the Rhum ultrabasic rocks. BS raised two questions which we answer below.

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33

Rottura, Alessandro, Alfredo Caggianelli, Raffaellamaria Campana y Aldo Del Moro. "Petrogenesis of Hercynian peraluminous granites from the Calabrian Arc, Italy". European Journal of Mineralogy 5, n.º 4 (22 de julio de 1993): 737–54. http://dx.doi.org/10.1127/ejm/5/4/0737.

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34

Oun, Khaled M. "On the poikilitic nature of Jabal Al Hasawinah eudialyte". Mineralogical Magazine 55, n.º 381 (diciembre de 1991): 543–47. http://dx.doi.org/10.1180/minmag.1991.055.381.07.

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AbstractPoikilitic eudialyte outcrops in a strongly peralkaline phonolithic cumulo-dome in Jabal Al Hasawinah, Libya. Textural relationships reveal that the eudialyte has formed at a very late stage of the rock petrogenesis. Electron microprobe analyses confirm its volatile (hydrous) nature and low REE content.

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35

Janoušek, V., B. Bonin, W. J. Collins, F. Farina y P. Bowden. "About this title - Post-Archean Granitic Rocks: Petrogenetic Processes and Tectonic Environments". Geological Society, London, Special Publications 491, n.º 1 (2020): NP. http://dx.doi.org/10.1144/sp491.

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Granites (sensu lato) represent the dominant rock-type forming the upper–middle continental crust but their origin remains a matter of long-standing controversy. The granites may result from fractionation of mantle-derived basaltic magmas, or partial melting of different crustal protoliths at contrasting P–T conditions, either water-fluxed or fluid-absent. Consequently, many different mechanisms have been proposed to explain the compositional variability of granites ranging from whole igneous suites down to mineral scale. This book presents an overview of the state of the art, and envisages future avenues towards a better understanding of granite petrogenesis. The volume focuses on the following topics: compositional variability of granitic rocks generated in contrasting geodynamic settings during the Proterozoic to Phanerozoic Periods;main permissible mechanisms producing subduction-related granites;crustal anatexis of different protoliths and the role of water in granite petrogenesis; andnew theoretical and analytical tools available for modelling whole-rock geochemistry in order to decipher the sources and evolution of granitic suites.

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36

Wang, Mengtao y Xin Zhang. "Petrogenesis of Devonian and Permian Pegmatites in the Chinese Altay: Insights into the Closure of the Irtysh–Zaisan Ocean". Minerals 13, n.º 9 (25 de agosto de 2023): 1127. http://dx.doi.org/10.3390/min13091127.

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Owing to tectonic, magmatic, and metamorphic controls, pegmatites associated with different spatiotemporal distributions exhibit varying mineralisation characteristics. The petrogenesis of pegmatites containing rare metals can improve the understanding of geodynamic processes in the deep subsurface. In order to understand the difference of petrogenesis between Devonian and Permian pegmatites, zircon U-Pb geochronological and Hf-O isotope analyses were performed on samples of the Jiamanhaba, Amulagong, and Tiemulete pegmatites from the Chinese Altay. According to the results obtained, the Amulagong and Tiemulete pegmatites were formed during the Devonian, and samples that were analysed yielded zircon U-Pb ages of 373.0 ± 7.8 and 360 ± 5.2 Ma, respectively. Samples from these pegmatites produced εHf(t) values of 2.87–7.39, two-stage model ages of 900–1171 Ma and δ18O values of 9.55‰–15.86‰. These results suggest that the pegmatites were formed via an anatexis of mature sedimentary rocks deep in the crust. In contrast, the Jiamanhaba pegmatite was formed during the Permian, and its samples produced εHf(t) and δ18O values of 2.87–4.94 and 6.05‰–7.32‰, respectively, which indicate that the associated magma contained minor amounts of mantle/juvenile materials. The petrogenesis of pegmatites containing rare metals can reveal tectonic settings of their formation. A combination of data that were generated in the present study and existing geochronological and Hf-O isotope data for felsic igneous and sedimentary rocks in the Chinese Altay shows that the εHf(t) sharply increased while the δ18O suddenly decreased between Late Carboniferous and Early Permian. These changes highlight a tectonic transformation event during this critical period. This tectonic event promoted mantle–crustal interactions, and thus, it was probably linked to assemblages of the Altay orogen and the Junggar Block. The present study provides evidence that the Irtysh–Zaisan Ocean probably closed during the Late Carboniferous (~300 Ma).

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37

Salkić, Zehra, Elvir Babajić, Alisa Babajić, Vedran Pobrić y Aldin Bešić. "PETROGENESIS OF THE MAGLAJ VOLCANICS, CENTRAL BOSNIA". Archives for Technical Sciences 1, n.º 11 (1 de octubre de 2014): 7. http://dx.doi.org/10.7251/afts.2014.0611.007s.

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38

Zheng, Yongfei. "Does the Mantle Contribute to Granite Petrogenesis?" Journal of Earth Science 33, n.º 5 (octubre de 2022): 1320. http://dx.doi.org/10.1007/s12583-022-1747-5.

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39

Smith, Diane R. y William P. Leeman. "Petrogenesis of Mount St. HElens dacitic magmas". Journal of Geophysical Research: Solid Earth 92, B10 (10 de septiembre de 1987): 10313–34. http://dx.doi.org/10.1029/jb092ib10p10313.

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40

Chesner, C. A. "Petrogenesis of the Toba Tuffs, Sumatra, Indonesia". Journal of Petrology 39, n.º 3 (1 de marzo de 1998): 397–438. http://dx.doi.org/10.1093/petroj/39.3.397.

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41

Crossley, S. D., N. G. Lunning, R. G. Mayne, T. J. McCoy, S. Yang, M. Humayun, R. D. Ash, J. M. Sunshine, R. C. Greenwood y I. A. Franchi. "Experimental insights into Stannern-trend eucrite petrogenesis". Meteoritics & Planetary Science 53, n.º 10 (22 de mayo de 2018): 2122–37. http://dx.doi.org/10.1111/maps.13114.

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42

Dawson, J. B. "Chapter 8 Regional comparisons, petrochemistry and petrogenesis". Geological Society, London, Memoirs 33, n.º 1 (2008): 79–89. http://dx.doi.org/10.1144/m33.8.

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43

Sarkhoshi A, عادل, مهراج Aghazadeh M y علیرضا Javanshir A. "Petrogenesis of NW of Bam Volcanic Rocks". Kharazmi Journal of Earth Sciences 1, n.º 2 (1 de febrero de 2016): 155–78. http://dx.doi.org/10.29252/gnf.1.2.155.

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44

MACDONALD, R., G. R. DAVIES, B. G. J. UPTON, P. N. DUNKLEY, M. SMITH y P. T. LEAT. "Petrogenesis of Silali volcano, Gregory Rift, Kenya". Journal of the Geological Society 152, n.º 4 (julio de 1995): 703–20. http://dx.doi.org/10.1144/gsjgs.152.4.0703.

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45

Wilson, Marjorie. "REVIEW OF IGNEOUS PETROGENESIS: AGLOBAL TECTONIC APPROACH". Terra Nova 1, n.º 2 (marzo de 1989): 218–22. http://dx.doi.org/10.1111/j.1365-3121.1989.tb00357.x.

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46

Aurisicchio, Carlo, Rosangela Bocchio, Giuseppe Liborio y Annibale Mottana. "Petrogenesis of the eclogites from Soazza, Switzerland". Chemical Geology 50, n.º 1-3 (agosto de 1985): 47–63. http://dx.doi.org/10.1016/0009-2541(85)90111-1.

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Bodinier, J. L., C. Dupuy y J. Dostal. "Geochemistry and petrogenesis of Eastern Pyrenean peridotites". Geochimica et Cosmochimica Acta 52, n.º 12 (diciembre de 1988): 2893–907. http://dx.doi.org/10.1016/0016-7037(88)90156-1.

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Taylor, Lawrence A. "Mare volcanism and basalt petrogenesis: An introduction". Geochimica et Cosmochimica Acta 56, n.º 6 (junio de 1992): 2153. http://dx.doi.org/10.1016/0016-7037(92)90182-i.

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Longhi, John. "Experimental petrology and petrogenesis of mare volcanics". Geochimica et Cosmochimica Acta 56, n.º 6 (junio de 1992): 2235–51. http://dx.doi.org/10.1016/0016-7037(92)90186-m.

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Stewart, Brian W., D. A. Papanastassiou y G. J. Wasserburg. "Sm-Nd chronology and petrogenesis of mesosiderites". Geochimica et Cosmochimica Acta 58, n.º 16 (agosto de 1994): 3487–509. http://dx.doi.org/10.1016/0016-7037(94)90100-7.

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