Добірка наукової літератури з теми "Upper mantle melting"
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Статті в журналах з теми "Upper mantle melting"
Hier-Majumder, Saswata, and Benoit Tauzin. "Pervasive upper mantle melting beneath the western US." Earth and Planetary Science Letters 463 (April 2017): 25–35. http://dx.doi.org/10.1016/j.epsl.2016.12.041.
Повний текст джерелаKOSTOPOULOS, D. K. "Melting of the Shallow Upper Mantle: A New Perspective." Journal of Petrology 32, no. 4 (August 1, 1991): 671–99. http://dx.doi.org/10.1093/petrology/32.4.671.
Повний текст джерелаSchiano, Pierre, Bernard Bourdon, Robert Clocchiatti, Dominique Massare, Maria E. Varela, and Yan Bottinga. "Low-degree partial melting trends recorded in upper mantle minerals." Earth and Planetary Science Letters 160, no. 3-4 (August 1998): 537–50. http://dx.doi.org/10.1016/s0012-821x(98)00109-5.
Повний текст джерелаWASYLENKI, L. E. "Near-solidus Melting of the Shallow Upper Mantle: Partial Melting Experiments on Depleted Peridotite." Journal of Petrology 44, no. 7 (July 1, 2003): 1163–91. http://dx.doi.org/10.1093/petrology/44.7.1163.
Повний текст джерелаXu, Man, Zhicheng Jing, Suraj K. Bajgain, Mainak Mookherjee, James A. Van Orman, Tony Yu, and Yanbin Wang. "High-pressure elastic properties of dolomite melt supporting carbonate-induced melting in deep upper mantle." Proceedings of the National Academy of Sciences 117, no. 31 (July 20, 2020): 18285–91. http://dx.doi.org/10.1073/pnas.2004347117.
Повний текст джерелаKimura, Takafumi, Kazuhito Ozawa, Takeshi Kuritani, Tsuyoshi Iizuka, and Mitsuhiro Nakagawa. "Thermal state of the upper mantle and the origin of the Cambrian-Ordovician ophiolite pulse: Constraints from ultramafic dikes of the Hayachine-Miyamori ophiolite." American Mineralogist 105, no. 12 (December 1, 2020): 1778–801. http://dx.doi.org/10.2138/am-2020-7160.
Повний текст джерелаGreen, T. H., E. H. Hauri, G. A. Gaetani, and J. Adam. "New calculations on water storage in the upper mantle, and implications for mantle melting models." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A215. http://dx.doi.org/10.1016/j.gca.2006.06.432.
Повний текст джерелаAiuppa, Alessandro, Federico Casetta, Massimo Coltorti, Vincenzo Stagno, and Giancarlo Tamburello. "Carbon concentration increases with depth of melting in Earth’s upper mantle." Nature Geoscience 14, no. 9 (August 5, 2021): 697–703. http://dx.doi.org/10.1038/s41561-021-00797-y.
Повний текст джерелаDasgupta, Rajdeep, and Marc M. Hirschmann. "Melting in the Earth's deep upper mantle caused by carbon dioxide." Nature 440, no. 7084 (March 2006): 659–62. http://dx.doi.org/10.1038/nature04612.
Повний текст джерелаKarato, S. "Does partial melting reduce the creep strength of the upper mantle?" Nature 319, no. 6051 (January 1986): 309–10. http://dx.doi.org/10.1038/319309a0.
Повний текст джерелаДисертації з теми "Upper mantle melting"
Burness, Sara. "Pyroxene stability within kimberlite magma in the upper mantle : an experimental investigation." Thesis, Stellenbosch : Stellenbosch University, 2015. http://hdl.handle.net/10019.1/96837.
Повний текст джерелаENGLISH ABSTRACT: Entrainment and assimilation of xenolithic material during kimberlite ascent is considered to be important in shaping the chemistry of the magma and fuelling magma ascent by driving CO2 exsolution. Previous, but as yet unpublished experimental work from Stellenbosch University has demonstrated that orthopyroxene has a key role in this. Orthopyroxene is a very rare xenocrystic constituent of kimberlite but makes up a considerable fraction of the entrained xenolithic material. The initial study used a natural kimberlite composition (ADF1) doped with a peridotite mineral suite (by weight); 88 % ADF1 5% olivine, 5% orthopyroxene and 2% garnet-spinel intergrowth as a starting composition. The subsequent high PT experiments (1100 to 1300°C and 2.0 to 3.5GPa) established that equilibrium orthopyroxene is stable at 1100°C above 2.5GPa, at 1200°C above 2.5GPa and at 1300°C between 2.0 and 3.5GPa. At lower pressures orthopyroxene is completely digested by the experimental melt by the reaction; Mg2Si2O6 (opx) = Mg2SiO4 (ol) + SiO2 (in liquid). In contrast, clinopyroxene is a common phase in kimberlite and often occurs as more than one generation of crystals. Xenocrystic clinopyroxene is dominated by diopside compositions. However, rare omphacite is sometimes also inherited from an eclogite source. The Omphacite, like orthopyroxene, displays textural evidence of severe disequilibrium and may also contribute to the evolution of kimberlitic melt. Thus, a second study produced experiments on the ADF1 kimberlite material at upper mantle PT conditions (1100 to 1300°C and 2.0 to 4.0GPa) as well as an omphacite doped starting material (ADF1+O). These experiments examine the behaviour of pyroxene in kimberlite magma including the influence this may have on magma buoyancy. Within this PT range omphacitic clinopyroxene breaks-down via complex multipart reactions. At 1100°C and 2.0GPa reaction textures around remnant omphacite suggest that omphacite melts incongruently in a complex reaction similar to: Omp + Melt = Ap + Cr-diop + SiO2-enriched Melt. At 1300°C omphacite melts completely and is perceived to produce peritectic Cr-diopside, calcium-rich olivine, carbonate in the melt as well as enrich the melt in SiO2. The melts produced by both the ADF1+O and ADF1 compositions at 1300°C and 4.0GPa are reduced in SiO2 content and have increased TiO2, Cr2O3, Al2O3, MnO, CaO, K2O and P2O5 compared to their respective starting compositions. However, significantly higher proportions of Ca, Na and Fe observed within the ADF1+O melt is a direct consequence of omphacite melting. The ADF1+O starting composition produced equilibrium orthopyroxene above 1100°C and 4.0GPa as well as at 1300°C above 2.0GPa. At lower pressure the orthopyroxene melts incongruently to form peritectic olivine and more silica-rich melt compositions. This digestion favours CO2 exsolution. The effect of orthopyroxene melting can be seen in the melt compositions produced by the peridotite doped starting material (ADF1+P) of the initial study. At 1300°C and 2.0GPa, ADF1+P produced a siliceous melt (37.0 wt.% SiO2) enriched in Al and alkalis compared to the starting ADF1+P composition. This behaviour is directly attributed to xenocrystic orthopyroxene melting at high temperature. In contrast, at the same PT the original kimberlite (ADF1) composition produces a melt with 28.9 wt.% SiO2 and high Ca and Mg contents. Overall, with an increase in pressure the melts become enriched in alkalis and Al2O3 as a direct result of xenocrystic pyroxene melting. In addition, increased pressure allows for a greater solubility of CO2 within the melt. This results in a lower SiO2 melt content and the increased stabilization of equilibrium silica-rich mineral phases (i.e. olivine and equilibrium orthopyroxene). Within the peridotite doped static system (unpublished) the mineral separates with an average crystal size of 115μm ±10μm were all effectively digested in less than 48hours. Similarly, the omphacite doped experiments consumed the 150μm (±10μm) xenocrysts in under 24 hours. Thus, it is suggested that xenocrystic pyroxene is unstable in these experimental kimberlitic melt compositions and is likely to be efficiently assimilated in less than 24 hours. These experimental melts most likely resemble those of natural systems under upper mantle PT conditions. Therefore, pyroxene melting increases the silica content of the melt which in turn drives CO2 exsolution and ascent.
AFRIKAANSE OPSOMMING: Meevoering en assimilasie van xenolitiese materiaal gedurenende kimberliet bestyging is beskou as belangrik in verband met die vorming van die chemie van die magma, en bevorder magma bestyging deur die aandrywing van CO2 ontmenging. Vorige, maar ongepubliseerde eksperimentele werk vanaf Stellenbosch Universiteit het gedemonstreer dat ortopirokseen ‘n sleutelrol hierin het, omrede ortopirokseen ‘n baie skaars xenokristiese bestanddeel van kimberliet is maar ‘n aansienlike fraksie van die meevoerde xenolitiese materiaal moet opmaak. Hierdie studie het ‘n natuurlike primere kimberliet komposisie (ADFI) gedoop met ‘n peridotiet mineraal reeks (per gewig); 88 % ADF1 5% olivien, 5% ortopirokseen en 2% granaat-spinel ingroeiing as begin komposisie gebruik. Die daaropvolgende hoë DT eksperimente (1100 tot 1300°C en 2.0 tot 3.5GPa) het vasgestel dat ewewigsortopirokseen stabiel is teen 1100°C bo 2.5GPa, 1200°C bo 2.5GPa en teen 1300°C vanaf 2.0 tot 3.5Gpa. Teen laer druk word ortopirokseen geheel verteer deur die eksperimentele smelting volgens die reaksie Mg2Si2O6 (opx) = Mg2SiO4 (ol) + SiO2 (in vloeistof). In kontras hiermee is clinopirokseen algemeen in kiemberliet en kom dikwels voor as meer as een generasie se kristalle. Diopsiet komposisies domineer xenokristiese klinopirokseen. Seldsame omfasiet is tog somtyds ook geërf vanaf ‘n eklogiet bron. Die omfasiet, soos ortopirokseen, vertoon teksturuele bewys van ernstige disekwilibrium en mag ook bydra tot die evolusie van kimberlitiese smelt. Dus was daar addisionele eksperimente uitgevoer op die ADF1 kimberliet material teen hoër mantel DT kondisies (1100 tot 1300°C en 2.0 tot 4.0GPa), asook ‘n begin materiaal gedoop met omfasiet (ADF1+O). Hierdie eksperimente ondersoek die gedrag van pirokseen in kiemberliet magma, asook die invloed wat dit sal hê op die dryfvermoë van die magma. Binne hierdie DT reeks breek omfasitiese klinopirokseen af via komplekse multideel reaksie prosesse. Teen 1100°C en 2.0Gpa stel reaksie teksture rondom die oorblywende omfasiet voor dat omfasiet ongelykvormig smelt deur ‘n komplekse reaksie soortgelyk aan: Omp + Smelt = Ap + Cr-diop + SiO2-verrykde Smelt. Teen 1300°C smelt omfasiet volkome en is waargeneem om peritektiese Cr-diopsiet, kalsiumryke olivien en kalsiet te produseer, sowel as dat dit die smelt verryk in SiO2. Die smeltings geprodiseer deur die ADF1+O en ADF1 massa komposisies teen 1300°C en 4.0GPa is verlaag in SiO2 inhoud en bevat verhoogde TiO2, Cr2O3, Al2O3, MnO, CaO, K2O en P2O5 in vergelyking met die onderskeie begin komposisies. Aansienlike hoër proporsies van Ca, Na en Fe is egter waargeneem in die ADF1+O smelt en is ‘n direkte gevolg van die smelting van omfasiet. Die ADF1+O begin samestelling het ewewigsortopirokseen bo 1100°C en 4.0Gpa geproduseer en massa teen 1300°C en 2.0 tot 4.0GPa. Teen laer druk smelt hierdie pirokseen inkongruent om peritektiese olivien en meer silika-ryke smelt samestellings te vorm, en ontmeng CO2. Die effek van ortopirokseen smelting kan aanskou word in die smelt samestellings wat produseer is deur die begin materiaal wat gedoop is in peridotiet (ADF1+P), in die oorspronklike studie. Teen 1300°C en 2.0GPa het ADF1+P ‘n silikahoudende smelt (37.0 wt.% SiO2) produseer wat verryk is in Al en alkalies in vergelyking met die ADF1+P massa samestelling. Hierdie gedrag is direk toegeskryf aan die xenokristiese ortopirokseen wat smelt teen hoë temperatuur. In kontras hiermee, teen dieselfde DT kondisies produseer die oorspronklike kiemberliet (ADF1) massa ‘n smelt met 28.86 gewigspersentasie SiO2 en hoë Ca en Mg inhoud. In die algeheel word die smeltings verryk in alkalies en Al2O3 teen verhoogde druk as ‘n derekte gevolg van xenokristiese pirokseen smelting. Verder laat verhoogde druk toe vir hoër oplosbaarheid van CO2 in die smelt, wat lei tot laer SiO2 inhoud en ‘n toename in stabilisering van ewewigs silika-ryke mineraal fases (dws. olivien en ewewigsortopirokseen). In die peridotiet gedoopde statiese sisteem (ongepubliseerd), was die mineraal skeiding met ‘n gemiddelde kristal grootte van 115μm ±10μm almal effektief verteer in minder as 48 ure. Soortgelyk hieraan het die omfasiet gedoopde eksperimente die 150μm (±10μm) sade onder 24 ure verteer. Dus stel dit voor dat xenokristiese pirokseen in naatuurlike sisteme onstabiel is in kiemberlietiese smelt samestellings en sal waarskynlik geassimileer wees in miner as 24 ure en ‘n meer silica-ryke kiemberlietiese smelt samestelling produseer terwyl dit CO2, ontmenging en bestyging aandryf.
Freitas, Damien. "The transport properties of Earth’s upper mantle materials : insights from in situ HP-HT experiments." Thesis, Université Clermont Auvergne (2017-2020), 2019. http://www.theses.fr/2019CLFAC058.
Повний текст джерелаThe transport properties of mantle rocks are key parameters to qualitatively and quantitatively interpret direct and indirect geophysical information such as seismic velocities, heat fluxes and electromagnetic profiles across Earth’s and planetary interiors. The origins of upper mantle geophysical anomalies such as the Low Velocity Zone (70-150 km deep) and the Low Velocity Layer (350-410 km deep) are poorly known and require experimental constraints. In this PhD thesis, we have explored the electrical, seismic and thermal properties of realistic solid and partially molten peridotites via the development of geophysical in situ techniques. Performed at high pressures and temperatures in multi-anvil apparatus, our experiments allowed the characterization of the effect of melting on these different physical properties at mantle conditions. We performed the first experimental combination of electrical conductivity and sound wave velocity in a single multi-anvil experiment. Thanks to this technique, we reconciled electrical and seismic estimations of the melt fraction implied in the LVZ with 0.3-0.8 Vol.% of partial melting. The textural equilibration between melt and solid phases was found to be crucial for the comparison of laboratory estimations. We then realized the first reproduction of the dehydration melting process during the ascend of hydrous peridotites from the mantle transition zone to the upper mantle, between 12 and 14 GPa. Measurements during partial melting gave acoustic and electrical signals comparable to geophysical observations favoring partial melting explanation of the LVL anomaly. The implied melt fractions at upper mantle base were quantified to be moderate (<2 Vol.%). The chemical composition of produced melts confirmed the role of chemical filter of this melt layer located between upper and deep mantle. The calculated density confirmed the neutral buoyancy of the melt layer, making it a stable feature over geological times. Volatiles analyses and hydrogen transfer modeling confirmed this layer as a potential deep water reservoir and favored a bottom-up hydration of Earth’s upper mantle. Thermal diffusivity characterization techniques (Angström and pulse heating methods) were adapted to the LMV multi-anvil apparatus. Improved treatment procedures were elaborated for thermal transfer characterization under HP and HT conditions. The first thermal diffusivity characterization of glasses and melts at realistic mantle conditions were performed. In addition, thermal diffusivities of various samples (periclase, olivine, peridotite) were investigated with different structures (solid, solid+melt etc.) using Angström method
Gueddari, Khalid. "Approche géochimique et physico-chimique de la différenciation des éléments du groupe du platine (PGE) et de l'or dans le manteau supèrieur bético-rifain et dans les xénolites de péridotites sous continentales." Université Joseph Fourier (Grenoble), 1996. http://www.theses.fr/1996GRE10031.
Повний текст джерелаRosenthal, Anja. "Exploring the melting behaviour of the Earth's heterogeneous upper mantle." Phd thesis, 2009. http://hdl.handle.net/1885/151214.
Повний текст джерелаWasylenki, Laura Eileen. "Partial Melting of Depleted Peridotite in the Earth's Upper Mantle and Implications for Generation of Mid-Ocean Ridge Basalts." Thesis, 1999. https://thesis.library.caltech.edu/11860/1/wasylenki-le-1999.pdf.
Повний текст джерелаPeridotite in the earth's upper mantle undergoes polybaric, fractional melting as it rises adiabatically beneath mid-ocean spreading ridges. As liquid is continually extracted, peridotite becomes increasingly depleted in incompatible components. The amounts and compositions of partial melts of depleted peridotite are important parameters in models of MORB petrogenesis, but have not been well-constrained previously. I present partial melting experiments on a depleted peridotite composition at 10 kbar and 1250–1390°C. My experiments make use of small aggregates of glassy carbon particles into which partial melt is extracted at high temperature. I have been able to analyze low degree partial melts (<10%) and quantify the effects of incompatible element depletion on the melting behavior of peridotite. Special tests of the approach to equilibrium in this study confirm the validity of the aggregate melt extraction technique, which has sparked much debate in the literature (see Chapters 2 and 3 for details).
Melts of depleted peridotite differ in important ways from melts of fertile peridotite, mostly due to lower alkali contents and chemical consequences thereof. At low melt fractions, melts of depleted peridotite have less SiO₂, more CaO, and higher CaO/Al₂O₃ than melts of fertile peridotite at the same melt fraction. According to these results and others in the literature, solidus temperature is a linear function of incompatible major element content. Melt fraction at cpx-out is proportional to normative cpx in source peridotite.
Liquid compositions from this study are in good agreement with calculations using the quantitative models of Kinzler and Grove (1992a), Langmuir et al. (1992), and Ghiorso and Sack (1995). Calculations of polybaric, fractional melting of primitive mantle using the models of Langmuir et al. (1992) and Asimow (1997) indicate that about half of all liquid contributed to MORB is formed by partial melting of depleted peridotite.
The data presented in this thesis provide information about amounts and compositions of partial melts formed from depleted peridotite, an important upper mantle constituent beneath mid-ocean ridges, and can be used to improve quantitative models of MORB primary magma formation and further our understanding of MORB petrogenesis.
Balta, Joseph Brian. "1. Experimental Investigation of Hydrous Melting of the Earth’s Upper Mantle, and 2. Olivine Abundances and Compositions in Hawaiian Lavas." Thesis, 2010. https://thesis.library.caltech.edu/5494/9/Chapter0.pdf.
Повний текст джерела(1) The presence of small amounts of water dissolved within nominally-anhydrous minerals in the earth has significant effects on the chemistry of melting in the Earth’s mantle. Upwelling rock containing water will melt at greater depths than the same rock would if it were volatile-free, and the chemistry of these hydrous melts is expected to be quite different from that of anhydrous melts. We have developed new experimental techniques and applied them to melting under pressures where hydrous melting is of the greatest natural importance. We have also controlled the content of carbon, another volatile element, to produce melts from a range of compositions not previously sampled experimentally.
The liquid composition shows a number of interesting properties. Compared to anhydrous melts from the same pressure, it shows decreased modal olivine and increased silica content. Compared to carbon-containing experiments, it suggests that carbon interacts with water when both volatiles are present, and may act to oppose the effects of water. The presence of a hydrous liquid also has an important effect on the coexisting solid chemistry. High-aluminum clinopyroxenes are commonly observed at this pressure in anhydrous systems. However, in all of our volatile-containing experiments, the clinopyroxenes show a substantial decrease in aluminum content and an increase in calcium content. Many elements, including water, enter into the clinopyroxene structure by coupled substitution with aluminum, and thus reduced clinopyroxene aluminum content during natural melting will decrease the partitioning of these elements during melting.
(2) Variations in the modal abundance of olivine are the main mineralogical differences amongst typical Hawaiian lavas. A large quantity of olivine must crystallize from the Hawaiian parental liquids prior to eruption to produce the erupted lavas. The chemistry and abundance of these olivines reflects the behavior of the magmatic system in a number of ways. We have used the chemistry of these olivines and lavas to estimate the parental liquid compositions in Hawaiian volcanoes, to infer the relationship between the olivines and the lavas that host them, and to probe the evolution of Hawaiian volcanoes over time.
Kovács, Andrea. "Geochemie hornin svrchního pláště lokality Mohelno-Biskoupky." Master's thesis, 2010. http://www.nusl.cz/ntk/nusl-295840.
Повний текст джерелаКниги з теми "Upper mantle melting"
Vaughan, David. 3. Minerals and the interior of the Earth. Oxford University Press, 2014. http://dx.doi.org/10.1093/actrade/9780199682843.003.0003.
Повний текст джерелаЧастини книг з теми "Upper mantle melting"
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.
Повний текст джерелаWyllie, Peter J. "Experimental Limits for Melting in the Earth's Crust and Upper Mantle." In Geophysical Monograph Series, 279–301. Washington D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm014p0279.
Повний текст джерелаGrove, Timothy L., and Christy B. Till. "Melting the Earth's Upper Mantle." In The Encyclopedia of Volcanoes, 35–47. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-385938-9.00001-8.
Повний текст джерелаA. Abu El-Rus, Mohamed, Ali A. Khudier, Sadeq Hamid, and Hassan Abbas. "The Ampferer-Type Subduction: A Case of Missing Arc Magmatism." In Updates in Volcanology - Linking Active Volcanism and the Geological Record [Working Title]. IntechOpen, 2023. http://dx.doi.org/10.5772/intechopen.109406.
Повний текст джерелаA. El Bahariya, Gaafar. "An Overview on the Classification and Tectonic Setting of Neoproterozoic Granites of the Nubian Shield, Eastern Desert, Egypt." In Geochemistry. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.95904.
Повний текст джерелаRivers, Toby, and Richard A. Volkert. "Slow cooling in the metamorphic cores of Grenvillian large metamorphic core complexes and the thermal signature of the Ottawan orogenic lid." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(16).
Повний текст джерелаSwanson-Hysell, Nicholas L., Toby Rivers, and Suzan van der Lee. "The late Mesoproterozoic to early Neoproterozoic Grenvillian orogeny and the assembly of Rodinia: Turning point in the tectonic evolution of Laurentia." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(14).
Повний текст джерелаSmith, Alan L., M. John Roobol, Glen S. Mattioli, George E. Daly, and Joan E. Fryxell. "Providencia Island: A Miocene Stratovolcano on the Lower Nicaraguan Rise, Western Caribbean—A Geological Enigma Resolved." In Providencia Island: A Miocene Stratovolcano on the Lower Nicaraguan Rise, Western Caribbean—A Geological Enigma Resolved, 1–101. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.1219(01).
Повний текст джерелаТези доповідей конференцій з теми "Upper mantle melting"
Vaughn, Lochlan, Robert J. Stern, Jeffrey Ryan, and Julian A. Pearce. "AN ANIMATED EXPLANATION OF MANTLE MELTING AIMED AT UPPER DIVISION UNDERGRADUATES." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324229.
Повний текст джерелаWilliams, Helen, Simon Matthews, Hanika Rizo, and Oliver Shorttle. "Iron isotopes trace primordial magma ocean cumulates melting in the Earth’s upper mantle." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6434.
Повний текст джерелаStolper, E. M., and O. Shorttle. "MSA ROEBLING MEDAL LECTURE: THE EFFECTS OF SOLID-SOLID PHASE EQUILIBRIA AND PARTIAL MELTING ON THE OXYGEN FUGACITY OF THE UPPER MANTLE." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304520.
Повний текст джерела