Relevant bibliographies by topics / Petrogenesis

Academic literature on the topic 'Petrogenesis'

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Published: 4 June 2021
Last updated: 30 July 2024

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Journal articles on the topic "Petrogenesis"

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Janoušek, Vojtěch, and Jean-François Moyen. "Whole-rock geochemical modelling of granite genesis: the current state of play." Geological Society, London, Special Publications 491, no. 1 (February 6, 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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Leeman, William P. "Igneous petrogenesis." Geochimica et Cosmochimica Acta 61, no. 10 (May 1997): 2147. http://dx.doi.org/10.1016/s0016-7037(97)83223-1.

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

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Grove, T. L., and R. J. Kinzler. "Petrogenesis of Andesites." Annual Review of Earth and Planetary Sciences 14, no. 1 (May 1986): 417–54. http://dx.doi.org/10.1146/annurev.ea.14.050186.002221.

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Floss, Christine, Ghislaine Crozaz, Gordon McKay, Takashi Mikouchi, and Marvin Killgore. "Petrogenesis of angrites." Geochimica et Cosmochimica Acta 67, no. 24 (December 2003): 4775–89. http://dx.doi.org/10.1016/s0016-7037(03)00310-7.

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Canil, Dante. "The geochemistry of komatiites and basalts from the Deadman Hill area, Munro Township, Ontario, Canada." Canadian Journal of Earth Sciences 24, no. 5 (May 1, 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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Carnevale, Gabriele, Antonio Caracausi, Alessandra Correale, Laura Italiano, and Silvio G. Rotolo. "An Overview of the Geochemical Characteristics of Oceanic Carbonatites: New Insights from Fuerteventura Carbonatites (Canary Islands)." Minerals 11, no. 2 (February 15, 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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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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Roberts, Stephen, and Christopher Neary. "Petrogenesis of ophiolitic chromitite." Geological Society, London, Special Publications 76, no. 1 (1993): 257–72. http://dx.doi.org/10.1144/gsl.sp.1993.076.01.12.

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McGregor, V. R. "Igneous Petrogenesis. Marjorie Wilson." Journal of Geology 98, no. 5 (September 1990): 799. http://dx.doi.org/10.1086/629451.

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Dissertations / Theses on the topic "Petrogenesis"

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Colgan, Elizabeth Anne. "Petrogenesis of the Eshowe melilitites." Master's thesis, University of Cape Town, 1992. http://hdl.handle.net/11427/17331.

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The Eshowe melilitites intruded marginal cratonic crust at approximately 80my. Their intrusion followed after a long period of extensive rift tectonism associated with the breakup of Gondwanaland. The intrusives represent the final phase of alkaline and basaltic magmatism that commenced at about 200my. This magmatism was probably related to mantle processes responsible for the continental fragmentation and was controlled by a fluctuating mantle thermal regime. The Eshowe melilitites intrude an area of attenuated crust in an essentially rift valley setting. Petrological, and chemical evidence suggest that the Emtilombo melilitite does not represent crystallisation of a primary magma. The magma was generated in the asthenosphere but reacted with incompatible element and probably CO₂ and H₂O enriched lithosphere and perhaps crustal sources on its way to the surface. The Emtilombo melilitite contains microxenoliths of mantle derived spinel peridotite and of a suite of dunitic rocks that are believed to be high pressure cumulates of earlier alkaline magmas. These latter trapped melts would have introduced metasomatising agents into the lithosphere. The dunitic melts are believed to represent earlier intrusions related to the Eshowe alkaline volcanism. The chemistry of the olivine phenocrysts and microphenocrysts and complex zonation patterns on olivine xenocrysts (macrocryst and some complex phenocrysts) suggest the Emtilombo magma formed by mixing of several batches of melt. The 'parental magmas' to the Eshowe occurrences are therefore considered to consist of a mixture of asthenospheric and lithospheric components and a variety of different melts. The 'parental magma' to the Emtilombo dyke was an incompatible element enriched ultramafic melt that contained microxenoliths of spinel lherzolite and the dunitic suite of rocks. Changing oxygen fugacities are believed to be controlled by a loss of volatiles at relatively shallow depths in the mantle or lower crust. These changes are reflected by the spinel chemical trends and perovskite crystallisation. The change occurred after complex zonation patterns had developed on the olivines. The microphenocryst olivines are believed to be the only population of grains that crystallised from the Emtilombo 'parental magma'. Mode of emplacement of the melilitites is probably influenced by the nature and volume of magma in the intrusion, its volatile content, and to some extent the nature of the country rock. The Eshowe melilitites show a wide variety of intrusive modes and also demonstrate how late stage processes, possibly during or post consolidation, influence the geochemistry of the rock type.
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Wang, Yan. "Petrogenesis of permian flood basalts and mafic-ultramafic intrusions in the Jinping (SW China) and Song Da (Northern Vietnam) districts." Click to view the E-thesis via HKUTO, 2006. http://sunzi.lib.hku.hk/hkuto/record/B37758743.

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Ozdemir, Yavuz. "Volcanostratigraphy And Petrogenesis Of Suphan Stratovolcano." Phd thesis, METU, 2011. http://etd.lib.metu.edu.tr/upload/12613051/index.pdf.

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This study is concerned with volcanostratigraphic and petrologic evolution of the Sü
phan, which is a 4050 m high Quaternary stratovolcano in eastern Anatolia. The eruptive products of Sü
phan Stratovolcano, including transitional mildly alkaline to calc-alkaline rocks, are lavas, domes and pyroclastics ranging in composition from basalts to rhyolites. Ar-Ar age data from different levels of the volcanostratigrafic succession yield a range of 0.76-0.06 Ma. Textural features, wide temperature ranges obtained for intermediate members, and the linear trends of whole-rock geochemistry are strongly suggestive of magma mixing in the evolution of Sü
phan volcanics. Presence of crystal clots in many lavas suggests that cogenetic plutonic rocks were also involved in the mixing process. Comparison of whole-rock, melt inclusion and glass chemistry data of Sü
phan to data from experimental studies reported in literature indicate that the melt inclusions describe true liquid lines of descent from a common hydrous parent at pressures of ~500 MPa. EC-AFC modeling of trace element and isotopic compositions reveals 2-8% crustal contamination in the differentiated lavas. REE modeling indicates that primitive rocks of Sü
phan volcanics were products of mixing of melts from spinel and garnet lherzolite sources, with contributions of 60% and 40%, respectively, in the mixture. A two-stage petrogenetic model is proposed for Suphan stratovolcano. Mantle- derived melts stall and undergo chemical differentiation in a deep hot zone in lower to mid-crust
variably evolved melts ascending from this zone are arrested and mixed at a shallow level where they construct a sub-volcanic magma reservoir beneath Suphan.
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Student, James John. "Silicate Melt Inclusions in Igneous Petrogenesis." Diss., Virginia Tech, 2002. http://hdl.handle.net/10919/28719.

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Silicate melt inclusions are ubiquitous in quartz phenocrysts, yet there are few studies of such inclusions from porphyry copper systems. A melt inclusion forms when magma is trapped in a growing phenocryst. If a phenocryst is able to preserve the original parent magma, then accurate information can be obtained for ancient volcanic systems. In recent igneous systems, melt inclusions are commonly preserved as optically clear homogeneous glass representative of magma stored at depth before eruption. Melt inclusions are difficult to recognize in quartz phenocrysts from porphyry copper system because they are crystalline and hidden by exsolved magmatic volatiles. The inclusions range in size from less than 5 to over 150 μm. In order to evaluate the magmatic contribution to economic mineralization, we conducted three separate studies to determine whether or not crystallized melt inclusions preserve representative samples of magma. The first study modeled the phase relationships that occur during equilibrium crystallization and melting of haplogranite magma trapped in quartz. Results from the model are similar to observations made during the heating of crystallized melt inclusions from porphyry copper systems. It is necessary to re-melt the crystal and volatile phases before chemical analysis. Micro-explosions caused by heating resulted in the loss of important chemical components. Our second study evaluated several microthermometric heating procedures using synthetic melt inclusions trapped at conditions similar to those inferred for porphyry copper systems. A synthetic hydrous melt was saturated with saline hydrothermal solutions allowing both melt and aqueous fluids to be trapped in quartz. Based on microthermometric measurements from these coeval melt and aqueous fluid inclusions we were able to predict the known trapping temperature and pressure of formation. This technique can be applied to natural samples to constrain trapping pressures and temperatures. It was found that slower heating rates could be used to avoid overheating and that heating under a confining pressure greatly minimizes the decrepitation of inclusions. The third study examined the copper concentrations in melt inclusions from the Red Mountain, Arizona porphyry copper system. Older andesite magma contains pyroxene with melt inclusions of higher copper concentrations compared to melt inclusions in quartz from quartz latite. The higher water concentrations in crystallized melt inclusions in the quartz, and abundant aqueous fluid inclusions indicates that the exsolution of water from the magma occurred prior to the trapping of melt inclusions in quartz. The lower water concentrations and the absence of aqueous fluid inclusions indicates that the andesite never reached the stage of water exsolution. The results obtained here are consistent with models that suggest that copper is extracted from the melt by saline magmatic fluids, producing a metal-charged hydrothermal solution and leaving behind a metal-depleted melt and serves to identify the potential contribution of melt inclusion studies to constrain the origin of ore metals in porphyry copper deposits.
Ph. D.
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Jurinski, Joseph B. "Petrogenesis of the Moosehorn igneous complex, Maine." Thesis, This resource online, 1990. http://scholar.lib.vt.edu/theses/available/etd-04072010-020130/.

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Brown, Elizabeth Ann. "Rhyolite Petrogenesis at Tower Mountain Caldera, OR." PDXScholar, 2017. https://pdxscholar.library.pdx.edu/open_access_etds/3997.

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Tower Mountain Caldera is the main feature of an Oligocene volcanic field located in the Umatilla National Forest, eastern Oregon. It is perfectly suited to investigate models of rhyolite petrogenesis as all of the important rock components for evaluating generation models are present in a single location and thus are presumably related; basalts, intermediate igneous rocks (which consist of older plutons and younger volcanic rocks, which are ~coeval with rhyolites), metamorphic basement rocks of significant grade, and rhyolites of varying composition. The formation of the caldera produced the Dale Tuff, which comprises the intra-caldera and outflow facies. 40Ar/39Ar dating places the age of the tuff at 32.66 ± 0.36 Ma. Post-caldera rhyolites erupted along apparent ring fractures and elsewhere. Radiometric U-Pb dating of zircons from three of these rhyolites yielded ages of 32.167 ± 0.020 Ma (#CH07a), 31.798 ± 0.012 Ma (#TM5), and 31.426 ± 0.016 Ma (#CH08a). All rhyolites at Tower Mountain range from low to high silica varieties. Some of the post-caldera rhyolites are chemically similar to the Dale Tuff, such as sample CH07a, and have compositions typical of rhyolites of calc-alkaline volcanic centers (I-type rhyolites), while others are similar to A-type rhyolites (CH08a and TM5). The ages indicate that the calc-alkaline rhyolites were followed by the A-type rhyolites. The petrogenetic relationships between the various rocks types were evaluated. Partial melt modeling based on experimental melts produced from crustal material indicates that batch partial melting of metamorphosed high silica crustal material modified by the addition of more primitive mafic material by assimilation/contamination is the most likely source for the Tower Mountain rhyolites.
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Wallace, Graeme M. B. "Petrogenesis of the McGerrigle plutonic complex, Gaspe, Quebec." Thesis, McGill University, 1988. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63877.

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Shaw, Andrew. "The petrogenesis of Hercynian granites, French massif central." Thesis, Birkbeck (University of London), 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.397092.

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Becker, Mona Louise. "Petrogenesis of the Springfield Granodiorite, southeast Pennsylvania Piedmont." Thesis, This resource online, 1996. http://scholar.lib.vt.edu/theses/available/etd-05092009-040419/.

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Wood, Patricia Ann. "Petrogenesis of the Spruce Pine pegmatites, North Carolina." Thesis, This resource online, 1996. http://scholar.lib.vt.edu/theses/available/etd-08222008-063320/.

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Books on the topic "Petrogenesis"

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Wilson, Marjorie. Igneous Petrogenesis. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-9388-0.

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Wilson, Marjorie, ed. Igneous Petrogenesis. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-1-4020-6788-4.

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Hibbard, M. J. Petrography to petrogenesis. Englewood Cliffs, N.J: Prentice Hall, 1995.

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Marakushev, Alekseĭ Aleksandrovich. Petrogenezis. Moskva: "Nedra", 1988.

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Bucher, Kurt. Petrogenesis of Metamorphic Rocks. Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg, 2011.

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Bucher, Kurt, and Martin Frey. Petrogenesis of Metamorphic Rocks. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-662-03000-4.

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Bucher, Kurt, and Rodney Grapes. Petrogenesis of Metamorphic Rocks. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-540-74169-5.

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Bucher, Kurt, and Martin Frey. Petrogenesis of Metamorphic Rocks. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-04914-3.

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Bucher, Kurt. Petrogenesis of Metamorphic Rocks. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-12595-9.

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1940-, Frey Martin, ed. Petrogenesis of metamorphic rocks. 6th ed. Berlin: Springer-Verlag, 1994.

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Book chapters on the topic "Petrogenesis"

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Su, Ben-Xun. "Petrogenesis." In Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication, 135–56. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-54262-6_7.

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Ghose, Naresh Chandra, Nilanjan Chatterjee, and Fareeduddin. "Petrogenesis." In A Petrographic Atlas of Ophiolite, 79–83. New Delhi: Springer India, 2013. http://dx.doi.org/10.1007/978-81-322-1569-1_6.

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Wilson, Marjorie. "Relation of present-day magmatism to global tectonic processes." In Igneous Petrogenesis, 3–12. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_1.

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Wilson, Marjorie. "Continental tholeiitic flood basalt provinces." In Igneous Petrogenesis, 287–323. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_10.

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Wilson, Marjorie. "Continental rift zone magmatism." In Igneous Petrogenesis, 325–74. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_11.

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Wilson, Marjorie. "Potassic magmatism within Continental plates." In Igneous Petrogenesis, 375–416. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_12.

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Wilson, Marjorie. "Geochemical characteristics of igneous rocks as petrogenetic indicators." In Igneous Petrogenesis, 13–35. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_2.

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Wilson, Marjorie. "Partial melting processes in the Earth’s upper mantle." In Igneous Petrogenesis, 37–72. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_3.

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Wilson, Marjorie. "Processes which modify the composition of primary magmas." In Igneous Petrogenesis, 73–98. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_4.

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Wilson, Marjorie. "Mid-ocean ridges." In Igneous Petrogenesis, 101–50. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-94-010-9388-0_5.

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Conference papers on the topic "Petrogenesis"

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Yaxley, Gregory. "Petrogenesis of carbonatites." In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.14430.

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Huang, Hui. "Petrogenesis of high silica granites." In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.17891.

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Cronberger, Karl, and Clive R. Neal. "KREEPY MOON ROCKS: KREEP BASALT PETROGENESIS." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-312847.

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R. Backeberg, Nils. "Petrogenesis of the False Bay Dyke Swarm." In 11th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.241.backeberg_abstract.

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Taylor, Kaitlin C., Allison Beth Charney, and Randolph Steinen. "PETROGENESIS OF LAMPROPHYRES IN THE WALLINGFORD QUADRANGLE." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328386.

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Ismail, Taufik, Dini Nurfiani, Aditya Pratama, Mirzam Abdurrachman, Windi Anarta Draniswari, Idham Andri Kurniawan, and Wilfridus Ferdinando Supriyadi Banggur. "Petrogenesis study of Anak Krakatau volcanic rock." In THE 3RD INTERNATIONAL CONFERENCE ON NATURAL SCIENCES, MATHEMATICS, APPLICATIONS, RESEARCH, AND TECHNOLOGY (ICON-SMART2022): Mathematical Physics and Biotechnology for Education, Energy Efficiency, and Marine Industries. AIP Publishing, 2024. http://dx.doi.org/10.1063/5.0212510.

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O'Neill, Hugh, Laura Miller, Andrew J. Berry, and Charles Le Losq. "Petrogenesis of Basanite-Nephelinite Glasses from Early Kilauea." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1965.

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Austin, Tomoyo, Rodney V. Metcalf, and Brenda J. Buck. "METASOMATIC MICROTEXTURES AND THE PETROGENESIS OF AMPHIBOLE ASBESTOS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281939.

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Kerrigan, Ryan J. "PETROGENESIS OF ULTRAMAFIC BODIES IN THE PENNSYLVANIAN PIEDMONT." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302540.

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Giri, Rohit, and N. V. Chalapathi Rao. "Petrogenesis of Ultrapotassic Lamprophyre in Central Indian Tectonic Zone, Madhya Pradesh: An Insight to Petrogenesis of Lamprophyres of Central India." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.836.

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Reports on the topic "Petrogenesis"

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Brown, Elizabeth. Rhyolite Petrogenesis at Tower Mountain Caldera, OR. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.5881.

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Kieffer, M. Developing apatite chemistry as indicator for petrogenesis and mineral exploration. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329168.

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Whalen, J. B., and C. Gariepy. Petrogenesis of the Mcgerrigle Plutonic Complex, Gaspe, Quebec : a Preliminary Report. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120371.

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Azadbakht, Z., N. Rogers, D. R. Lentz, and C. R. M. McFarlane. Petrogenesis and associated mineralization of Acadian related granitoids in New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/313658.

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Nadeau, L., P. Brouillette, and J. Bédard. Geochemistry and petrogenesis of the Lapeyrère gabbronorite, south-central Grenville Province, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209526.

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Chai, G., R. Eckstrand, and C. Gregoire. Platinum group element concentrations in the Sudbury Rocks, Ontario - an indicator of petrogenesis. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134256.

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Sexton, A. J., and A. A. Cotie. Petrogenesis and economic geology of the Sporting Mountain pluton, Cape Breton Island, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120204.

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Palmer, E. M., C. R. M. McFarlane, D. R. Lentz, and H. Falck. Gold mineralization in the Cantung W-skarn deposit, Northwest Territories: an examination of distribution, mineralogy, and petrogenesis. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296480.

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Ali, H. M., and M. O. Nassief. Geochemical characteristics and petrogenesis of the Ophiolite sequence rocks from drill hole CY-4, Troodos complex, Cyprus. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127330.

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Carson, H. J. E., C. M. Lesher, and M. G. Houlé. Geochemistry and petrogenesis of the Black Thor intrusive complex and associated chromite mineralization, McFaulds Lake greenstone belt, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296681.

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