Relevant bibliographies by topics / Magmax

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Magmax'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Magmax.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Magmax"

1

Flannery, John, Rebecca Moore, Laura Marsella, Katie Harris, Martin Ashby, Paulina Rajko-Nenow, Helen Roberts, Simon Gubbins, and Carrie Batten. "Towards a Sampling Rationale for African Swine Fever Virus Detection in Pork Products." Foods 9, no. 9 (August 20, 2020): 1148. http://dx.doi.org/10.3390/foods9091148.

Full text
Abstract:
African swine fever (ASF) is a highly lethal disease of pigs caused by the ASF virus (ASFV), which presents a serious threat to global food security. The movement of contaminated pork products has previously been postulated as contributing to the introduction of ASF into new areas. To evaluate the performance of ASFV detection systems in multi-component pork products, we spiked sausage meat with four different ASFV-containing materials (ASFV cell culture, pork loin, meat juice and bone marrow). DNA was extracted using two manual systems (MagMAX CORE, Qiagen) and one automated (MagMAX CORE) one, and three qPCR assays (VetMAX, King, UPL) were used. The performance of the DNA extraction systems was as follows; automated MagMAX > manual MagMAX > manual Qiagen. The commercial VetMAX qPCR assay yielded significantly lower CT values (p < 0.001), showing greater sensitivity than the World Organization for Animal Health (OIE)-prescribed assays (King, UPL). Detection probability was the highest for matrices contaminated with bone marrow compared with pork loin or meat juice. An estimated minimum sample size of one 1-g sample is sufficient to detect ASFV in a homogenous pork product if bone marrow from infected pigs comprises 1 part in 10,000. We demonstrated that existing ASFV detection systems are appropriate for use in a food-testing capacity, which can provide an additional control measure for ASF.
APA, Harvard, Vancouver, ISO, and other styles
2

Fang, Xingwang, Roy C. Willis, Angela Burrell, Kurt Evans, Quoc Hoang, Weiwei Xu, and Mangkey Bounpheng. "Automation of Nucleic Acid Isolation on KingFisher Magnetic Particle Processors." JALA: Journal of the Association for Laboratory Automation 12, no. 4 (August 2007): 195–201. http://dx.doi.org/10.1016/j.jala.2007.05.001.

Full text
Abstract:
We describe automated nucleic acid (NA) isolation from diverse sample types using MagMAX kits (Ambion, Inc.) on KingFisher Magnetic Particle Processors (Thermo Scientific). The MagMAX-96 Blood RNA Isolation Kit is designed for total RNA isolation from whole blood from several species, without white blood cell fractionation, in about 45 min (including genomic DNA removal). The MagMAX-96 Total RNA Isolation Kit is designed for total RNA isolation from up to 2 × 10 6 cultured cells and up to 10-mg tissue. The isolated total RNA is highly intact and pure, ready to use in downstream applications such as microarray analysis or real-time reverse transcription (RT)-PCR for gene expression profiling or pathogen detection. The MagMAX-96 Viral RNA Isolation Kit is designed for viral RNA and DNA isolation from cell free or nearly cell-free samples such as swabs, serum, and plasma; it takes about 15 min. Total NA of high quality and purity is recovered at >75% efficiency, providing high sensitivity for pathogen detection by real-time RT-PCR. Unlike automated liquid handling systems that move reagents into and out of a single well of a multiwell plate to perform the different steps of an RNA isolation procedure, the KingFisher Magnetic Particle Processors use permanent magnetic rods to collect magnetic beads from solution and release them into another well containing reagent for the subsequent step of the procedure. The effectiveness of bead collection and transfer lead to superior washing and elution efficiency, as well as rapid processing. It is a very effective strategy for automation of magnetic-bead-based NA isolation kits. (JALA 2007; 12:195–201)
APA, Harvard, Vancouver, ISO, and other styles
3

Soldatova, Kristina I., Oleg Ivanovich Kit, Roman E. Tolmakh, Liubov Yu Vladimirova, and Denis S. Kutilin. "Cancer-testis gene-expression features in various tumors." Journal of Clinical Oncology 37, no. 15_suppl (May 20, 2019): e14260-e14260. http://dx.doi.org/10.1200/jco.2019.37.15_suppl.e14260.

Full text
Abstract:
e14260 Background: Cancer-testis antigens (CTA) can be an effective target for immunotherapy. Immunotherapeutic approaches targeting CTA in breast cancer (BC), endometrial cancer (EC), ovarian cancer (OC), and colon cancer (CRC) are in the incipient stages of development. The purpose of our study was screening of CTA specific for BC, EC, OC and CRC, based on an analysis of transcriptional profiles of CT-genes. Methods: Tumor and intact tissues of the breast, uterus, ovaries and colon were studied in 35, 30, 20 and 60 patients, respectively. RNAs were isolated using the method described by Chomczynski and Sacchi (2006). The REVERTA-L reagent kit was used for the cDNA synthesis. Relative expression of 16 genes ( MAGEA1, MAGEA2, MAGEA3, MAGEA4, MAGEB1, MAGEB2, GAGE1, GAGE3, GAGE4, MAGEC1, BAGE, XAGE3, NYESO1, SSX2, SCP1, PRAME1) was determined by Real-Time qPCR (with GAPDH and GUSB as reference genes). Statistical analysis was performed using the Mann-Whitney test. Results: BC patients showed significantly (p < 0.005) increased expression of MAGEA3, MAGEA4 and GAGE3 in tumor tissues compared to normal ones; EC patients - significantly (p < 0.05) increased expression of MAGEA1, MAGEA2, MAGEA4, MAGEB2, GAGE3, NY-ESO1, SCP1 and PRAME1 in tumor tissues compared to normal ones; OC patients - significantly (p < 0.05) increased expression of MAGEB1, MAGEB2, GAGE1, NY-ESO1 and decreased expression of MAGEA3, MAGEA4, GAGE3, GAGE4, XAGE3, SSX2, SCP1 and PRAME1; CRC patients - significantly (p < 0.05) increased expression of SSX2 and PRAME1, together with decreased BAGE expression, in tumors compared to normal tissues. Conclusions: Analysis of the transcriptional activity of CT-genes revealed the most common diagnostic markers and immunotherapeutic targets for every malignancy: in BC - MAGEA3, MAGEA4 and GAGE3, in EC - MAGEA1, MAGEA2, MAGEA4, MAGEB2, GAGE3, NY-ESO1, SYCP1 and PRAME1, in OC - MAGEB1, MAGEB2, GAGE1 and NY-ESO, in CRC - SSX2 and PRAME1.
APA, Harvard, Vancouver, ISO, and other styles
4

Sevilla, Iker A., Joseba M. Garrido, Elena Molina, María V. Geijo, Natalia Elguezabal, Patricia Vázquez, and Ramón A. Juste. "Development and Evaluation of a Novel Multicopy-Element-Targeting Triplex PCR for Detection of Mycobacterium avium subsp. paratuberculosis in Feces." Applied and Environmental Microbiology 80, no. 12 (April 11, 2014): 3757–68. http://dx.doi.org/10.1128/aem.01026-14.

Full text
Abstract:
ABSTRACTThe enteropathy called paratuberculosis (PTB), which mainly affects ruminants and has a worldwide distribution, is caused byMycobacterium aviumsubsp.paratuberculosis. This disease significantly reduces the cost-effectiveness of ruminant farms, and therefore, reliable and rapid detection methods are needed to control the spread of the bacterium in livestock and in the environment. The aim of this study was to identify a specific and sensitive combination of DNA extraction and amplification to detectM. aviumsubsp.paratuberculosisin feces. Negative bovine fecal samples were inoculated with increasing concentrations of two different bacterial strains (field and reference) to compare the performance of four extraction and five amplification protocols. The best results were obtained using the JohnePrep and MagMax extraction kits combined with an in-house triplex real-time PCR designed to detect IS900, ISMap02(an insertion sequence ofM. aviumsubsp.paratuberculosispresent in 6 copies per genome), and an internal amplification control DNA simultaneously. These combinations detected 10M. aviumsubsp.paratuberculosiscells/g of spiked feces. The triplex PCR detected 1 fg of genomic DNA extracted from the reference strain K10. The performance of the robotized version of the MagMax extraction kit combined with the IS900and ISMap02PCR was further evaluated using 615 archival fecal samples from the first sampling of nine Friesian cattle herds included in a PTB control program and followed up for at least 4 years. The analysis of the results obtained in this survey demonstrated that the diagnostic method was highly specific and sensitive for the detection ofM. aviumsubsp.paratuberculosisin fecal samples from cattle and a very valuable tool to be used in PTB control programs.
APA, Harvard, Vancouver, ISO, and other styles
5

Ha, Trang, and Valentina Harizanov. "Orders on magmas and computability theory." Journal of Knot Theory and Its Ramifications 27, no. 07 (June 2018): 1841001. http://dx.doi.org/10.1142/s0218216518410018.

Full text
Abstract:
We investigate algebraic and computability-theoretic properties of orderable magmas. A magma is an algebraic structure with a single binary operation. A right order on a magma is a linear ordering of its domain, which is right-invariant with respect to the magma operation. We use tools of computability theory to investigate Turing complexity of orders on computable orderable magmas. A magma is computable if it is finite, or if its domain can be identified with the set of natural numbers and the magma operation is computable. Interesting orderable magmas that are not even associative come from knot theory.
APA, Harvard, Vancouver, ISO, and other styles
6

Andrade, Valéria C. C., André L. Vettore, Manuella S. S. Almeida, José S. R. Oliveira, Maria de Lourdes L. F. Chauffaille, Mihoko Yamamoto, Adagmar Andriolo, et al. "Prognostic Impact of Cancer Testis Antigens Expression in Advanced Stage Multiple Myeloma Patients." Blood 110, no. 11 (November 16, 2007): 4733. http://dx.doi.org/10.1182/blood.v110.11.4733.4733.

Full text
Abstract:
Abstract Background: Cancer testis antigens have become the most extensively studied antigen group in the field of tumor immunology. Aims: This study aims to analyze global expression of 14 CT (cancer/testis) antigens in MM to identify possible prognostic markers and therapeutic targets. Patients and Methods: The expression of MAGEA1, MAGEA2, MAGEA3/6, MAGEA4, MAGEA10, MAGEA12, BAGE1, MAGEC1/CT7, GAGE family, LAGE-1, PRAME, NY-ESO-1, SPA17 and SSX1 was studied by RT-PCR in: 15 normal tissues, one pool of 10 normal bone marrow samples, three normal tonsils and bone marrow aspirates from six normal donors, three monoclonal gammophaties of undetermined significance (MGUS), five solitary plasmacytomas, 39 MM samples (95% advanced stage) and MM cell line U266. CodeLink Human UniSet I Bioarrays 10,000 genes was used for arrays analyses. Results: SPA17 was positive in all normal tissues and was excluded for further analyses. MAGEC1/CT7 was positive in bone marrow aspirates from one MGUS and in one plasmacytoma. U266 cell line was positive for all CT antigens, except SSX1. The frequencies of CT antigens expression in MM patients were: MAGEC1/CT7 = 30/39 (77%); LAGE-1 = 19/39 (49%); MAGEA3/6 = 16/39 (41%); MAGEA2 = 14/39 (36%); GAGE family = 13/39 (33%); NY-ESO-1 = 13/39 (33%); BAGE-1 = 12/39 (28%); MAGEA1 = 10/39 (26%); PRAME = 9/39 (23%); SSX-1 = 10/39 (26%); MAGEA12 = 8/39 (20.5%); MAGEA4 and MAGEA10 = 0%. Cox’s regression model showed that GAGE family positivity and number of positive CT antigens > 6 were independent prognostic factors when all patients were analyzed. However, MAGEC1/CT7 expression was the only independent prognostic factor when non-transplanted patients where analyzed. Three samples predominantly positive (> 6) and three samples predominantly negative (0 or 1) for the 13 analyzed CT antigens were submitted to microarrays analyses. 147 genes were overexpressed in predominantly positive CT antigens samples. Conclusions: Based on our findings, MAGEC1/CT7, MAGEA3/6 and LAGE-1 seem good candidates for immunotherapy, since together they are overexpressed in 85% of our MM cases. Besides, GAGE family expression, number of CT antigens > 6 and MAGEC1/CT7 seem to have impact on MM prognosis. Also, the results of arrays analyses corroborate the hypothesis that MM can be separate in two groups: predominantly positive and predominantly negative for CT antigens, meaning that these antigens may have important role for MM biology.
APA, Harvard, Vancouver, ISO, and other styles
7

Wiebe, R. A. "Mafic-silicic layered intrusions: the role of basaltic injections on magmatic processes and the evolution of silicic magma chambers." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 233–42. http://dx.doi.org/10.1017/s0263593300006647.

Full text
Abstract:
ABSTRACT:Plutonic complexes with interlayered mafic and silicic rocks commonly contain layers (1–50 m thick) with a chilled gabbroic base that grades upwards to dioritic or silicic cumulates. Each chilled base records the infusion of new basaltic magma into the chamber. Some layers preserve a record of double-diffusive convection with hotter, denser mafic magma beneath silicic magma. Processes of hybridisation include mechanical mixing of crystals and selective exchange of H2O, alkalis and isotopes. These effects are convected away from the boundary into the interiors of both magmas. Fractional crystallisation aad replenishment of the mafic magma can also generate intermediate magma layers highly enriched in incompatible elements.Basaltic infusions into silicic magma chambers can significantly affect the thermal and chemical character of resident granitic magmas in shallow level chambers. In one Maine pluton, they converted resident I-type granitic magma into A-type granite and, in another, they produced a low-K (trondhjemitic) magma layer beneath normal granitic magma. If comparable interactions occur at deeper crustal levels, selective thermal, chemical and isotopic exchange should probably be even more effective. Because the mafic magmas crystallise first and relatively rapidly, silicic magmas that rise away from deep composite chambers may show little direct evidence (e.g. enclaves) of their prior involvement with mafic magma.
APA, Harvard, Vancouver, ISO, and other styles
8

Thirumalapura, Nagaraja R., Willard Feria, Eric Hue, Corey Zellers, and Deepanker Tewari. "Evaluation of a high-throughput nucleic acid extraction method for the detection of Mycobacterium avium subsp. paratuberculosis in bovine fecal samples by PCR." Journal of Veterinary Diagnostic Investigation 33, no. 2 (February 1, 2021): 375–78. http://dx.doi.org/10.1177/1040638721991118.

Full text
Abstract:
Johne’s disease (paratuberculosis) is an economically important disease of cattle worldwide. The disease is caused by Mycobacterium avium subsp. paratuberculosis (MAP), a fastidious gram-positive bacterium. PCR is increasingly used in diagnostic laboratories for the detection of MAP in fecal samples given the rapid test turnaround time and sensitivity and specificity comparable to fecal culture. However, efficient extraction of DNA for sensitive detection of MAP by PCR is affected by the complex lipid-rich cell wall of MAP and the presence of PCR inhibitors in feces. We evaluated a high-throughput nucleic acid extraction method (MagMAX core nucleic acid purification kit with mechanical lysis module) in conjunction with an hspX gene PCR for the detection of MAP from bovine fecal samples, which resulted in correct identification of all negative (13 of 13) and positive (35 of 35) proficiency test samples obtained from the National Veterinary Services Laboratories. In addition, all 6 negative and 50 of 51 positive diagnostic specimens tested were categorized correctly.
APA, Harvard, Vancouver, ISO, and other styles
9

Poli, G., S. Tommasini, and A. N. Halliday. "Trace element and isotopic exchange during acid-basic magma interaction processes." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 225–32. http://dx.doi.org/10.1017/s0263593300006635.

Full text
Abstract:
ABSTRACT:Interaction processes between acid and basic magmas are widespread in the Sardinia–Corsica Batholith. The resulting hybrid magmas are extremely variable and can be broadly divided into: (i) microgranular mafic enclaves with geochemical characteristics of both magmatic liquids and cumulates; (ii) basic gabbroic complexes with internal parts mainly formed by cumulates and with interaction zones developing only in the marginal parts; and (iii) basic septa with the form of discrete, lenticular-like bodies often mechanically fragmented in the host rock. Different styles of interaction, ranging from mixing to mingling, have been related to variations in several physicochemical parameterś, such as: (i) the initial contrast in chemical composition, temperature and viscosity; (ii) the relative mass fractions and the physical state of interacting magmas; and (iii) the static versus dynamic environment of interaction.A model is presented for the origin and history of interaction processes between basic and acid magmas based on the geochemical characteristics of hybrid magmas. Physico-chemical processes responsible for the formation of hybrid magmas can be attributed to: (i) fractional crystallisation of basic magma and contamination by acid magma; (ii) loss of the liquid phase from the evolving basic magma by filter pressing processes; (iii) mechanical mixing between basic and acid magmas; and (iv) liquid state isotopic diffusion during the attainment of thermal equilibrium.
APA, Harvard, Vancouver, ISO, and other styles
10

Heincz, Adrián, Elemér Pál-Molnár, Balázs Kiss, Anikó Bataki, Enikő Eszter Almási, and Luca Kiri. "Nyílt rendszerű magmás folyamatok: magmakeveredés, kristálycsere és kumulátum-recirkuláció nyomai a Ditrói alkáli masszívumban (Orotva, Románia)." Földtani Közlöny 148, no. 2 (June 10, 2018): 125–42. http://dx.doi.org/10.23928/foldt.kozl.2018.148.2.125.

Full text
Abstract:
A Tarniţa Komplexum a Keleti-Kárpátokban (Románia) felszínre bukkanó Ditrói alkáli masszívum északi területének jellemző ultramafikus és mafikus kőzetegyüttese. A komplexum Ny-i részén, az Orotva-patak és a Felső-Pietrăriei-patak összefolyásánál található mélységi magmás kőzettestben kialakított mesterséges feltárás egyedülálló betekintést enged az egykori magmatározóban zajlott, több magma között lejátszódott keveredési és elegyedési folya matokba, illetve az új magmabenyomulások során feltépett, korábban kikristályosodott magmás kőzetfragmen tumok bekeveredési folya mataiba. A feltárásban látható befogadó kőzetben (szürke, közép- és durvaszemcsés, irányított szövetű diorit) négy különböző keveredési kőzetzárvány (mafikus kőzetzárvány; földpátszemes kőzetzárvány; porfíros (földpátaggregátumos), mafikus kőzetzárvány és ultramafikus kőzetzárvány) és egy eltérő eredetű felzikus kőzetzárvány típus figyelhető meg. A keveredési kőzetzárványok modális összetételük alapján mezokrata és melanokrata dioritok, valamint piroxénhorn blenditek, a felzikus kőzetzárványok pedig hololeukokrata dioritok. A különböző magmák közötti keveredés (mingling) legfontosabb bélyege az egymással — és a befogadó kőzet ásványainak orientált elhelyezkedésével — párhuzamos, megnyúlt, finomszemcsés, lencse alakú kőzetzárványok meg jele nése. A szögletes felzikus xenolitok és ultramafikus kőzetzárványok korábbi kumulátumok recirkulációját felté telezik, amelyek a benyomuló magmával kerültek a magmatározóba. A keveredési kőzetzárványok mafikus pereme és a közelükben megfigyelhető „slírek” további fontos jellemzői a legalább két magma keveredése során kialakuló szerke ze teknek. A magmaelegyedés gyakori velejárója a kristálycsere (crystal transfer). A vizsgált ásványok számos esetben mutatnak olyan jellegzetes mikroszöveti bélyegeket, amelyek e kristálycsere-folyamathoz köthetők a benyomuló és a befogadó magma, illetve a benyomuló magma és a feltépett kumulátumok között: a különféle zónásságot mutató és különbözőzárványgazdag plagioklászok, az amfibolköpennyel rendelkező piroxének és a plagioklászokban megjelenő tűs apatit kristályok. A jelen tanulmányban bemutatott részletes petrográfiai vizsgálatok rávilágítanak a Ditrói alkáli masszívum magmatározóinak összetett és változatos fejlődéstörténetére, amelyben meghatározó szerepet játszottak a nyílt rendszerű magmás folyamatok.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Magmax"

1

Hunt, Emma J. "Magma chamber dynamics in the peralkaline magmas of the Kakortokite Series, South Greenland." Thesis, University of St Andrews, 2015. http://hdl.handle.net/10023/6900.

Full text
Abstract:
Understanding crystallisation in magma chambers is a key challenge for igneous petrology. It is particularly important to understand the origins of layering in peralkaline rocks, e.g. the kakortokite (nepheline syenite), Ilímaussaq Complex, S. Greenland, as these are commonly associated with high value multi-element economic deposits. The kakortokite is a spectacular example of macrorhythmic (>5 m) layering. Each unit consists of three layers comprising arfvedsonite-rich (sodic-amphibole) black kakortokite at the base, grading into eudialyte-rich (sodic-zirconosilicate) red kakortokite, then alkali feldspar- and nepheline-rich white kakortokite. Each unit is numbered -19 to +17 relative to a characteristic well-developed horizon (Unit 0), however there is little consensus on their development. This project applies a multidisciplinary approach through field observations combined with petrography, crystal size distributions (CSDs), mineral and whole rock chemistries on Units 0, -8 to -11 and a phonolite/micro-nephelinolite (“hybrid”) sequence that crosscuts the layered kakortokite. Textures and compositions are laterally consistent across outcrop and indicators of current activity are rare. CSDs indicate in situ crystallisation with gravitational settling as a minor process. Chemical discontinuities occur across unit boundaries. The layering developed through large-scale processes under exceptionally quiescent conditions. The discontinuities reflect open-system behaviour; units were formed by an influx of volatile-rich magma that initiated crystallisation in a bottom layer. Nucleation was initially suppressed by high volatile element concentrations, which decreased to allow for crystallisation of arfvedsonite, followed by eudialyte, then alkali feldspar and nepheline to form each tripartite unit. The chemistry of the hybrid indicates mixing between a primitive (sub-alkaline) magma and kakortokite. Thus injections of magmas of varying compositions occurred, indicating a complex plumbing system below current exposure. The lessons learned at Ilímaussaq, which is extremely well exposed and preserved, are relevant to understanding magma chamber dynamics in the more common instances of pervasively altered peralkaline rocks.
APA, Harvard, Vancouver, ISO, and other styles
2

Barr, Jay Arthur. "Primitive magmas of the Earth and Moon : a petrologic investigation of magma genesis and evolution." Thesis, Massachusetts Institute of Technology, 2010. http://hdl.handle.net/1721.1/62493.

Full text
Abstract:
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2010.
"September 2010." Cataloged from PDF version of thesis.
Includes bibliographical references.
Field studies, major and trace element geochemistry, isotopes, petrography, phase equilibrium experiments and thermodynamics are used investigate and understand primitive melts from the Earth and the Moon. Chapter 1 investigates spinifex orthopyroxene compositions from the komatiites of Commondale, South Africa, and uses phase equilibrium experiments to illustrate that the Commondale Komatiites were hydrous magmas when they were emplaced. Hydrous komatiites provide evidence for the existence of subduction zone volcanism during the Archean, and decreases the temperature required to explain komatiites volcanism, which is the major physical evidence used to determine the mantle potential temperature of the Archean. Chapter 2 uses phase equilibrium experiments investigate the origin of the Apollo 15 green glasses from the Moon. Garnet-lherzolite saturated experiments are used to calibrate a melting algorithm used to estimate the chemical compositions of melts of a primordial lunar mantle. Mixing models are used to reproduce the Apollo 15 green glass compositions. These models are consistent with primordial melts assimilating late stage lunar magma ocean cumulates to produce the green glasses. This provides evidence for the magma overturn hypothesis, as well as evidence that the lunar magma ocean may not have been whole moon. Chapter 3 uses phenocryst petrology, Os-isotopes, major and trace element geochemistry and petrography to argue for the formation of primitive magnesian andesites of Mt. Shasta and Mt. Lassen as primary mantle melts. Recent proposals that primitive magnesian andesites form by mixing dacites with subvolcanic peridotite are disproven. Samples of these lavas from newly discovered localities provide clear evidence for a mantle origin for these melts. Understanding the primitive melts present in the Cascade volcanoes will yield greater insight into the mantle processes involved in the plumbing of the sub-arc mantle. Chapter 4 develops a ternary regular solution model for Au-Pd-Fe alloys and uses this with Fe-exchange experiments to model the dependence of alloy composition on the oxygen fugacity. Au-Pd alloy capsules are essential to hydrous phase equilibrium studies at high-pressure and high-temperature, and the use of this model allows for the quantification of the oxygen fugacity of these experiments without compromising sample volume.
by Jay Arthur Barr.
Ph.D.
APA, Harvard, Vancouver, ISO, and other styles
3

Wayman, Matthew C. "The Transfer of Volatiles Within Interacting Magmas and its Effect on the Magma Mingling Process." Kent State University Honors College / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=ksuhonors1312924338.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Snyder, Darin C. "Processes and Time Scales of Differentiation in Silicic Magma Chambers: Chemical and Isotopic Investigations." Connect to this document online, 2005. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=miami1113844626.

Full text
Abstract:
Thesis (Ph. D.)--Miami University, Dept. of Geology, 2005.
Title from second page of PDF document. Document formatted into pages; contains [3], viii, 216 p. : ill. Includes bibliographical references (p. 151-159).
APA, Harvard, Vancouver, ISO, and other styles
5

Liu, Lei. "The link between convection and crystallization in a sub-axial magma chamber and heat output in a seafloor hydrothermal system." Thesis, Available online, Georgia Institute of Technology, 2007, 2007. http://etd.gatech.edu/theses/available/etd-07072007-142506/.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Pressi, Leonardo Frederico. "Evolução magmática do plúton Piracaia (SP): parâmetros físico-químicos e evidências de mistura entre magmas monzodioríticos e sieníticos." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-11032013-104316/.

Full text
Abstract:
O presente trabalho investiga processos de interação e mistura parcial de magmas monzodioríticos e sieníticos s.l. no Plúton Piracaia,(~ 580 Ma), que pertence à Província Granítica Itu, de caráter pós-orogênico. O Plúton Piracaia é uma intrusão alongada com cerca de 30 km2, formada por cinco unidades: Monzodioritos grossos (Mdr); Monzodioritos finos (Mdf); Monzonitos heterogêneos (Mh); Sienitos (Sie); quartzo sienitos e quartzo monzonitos (Qsie). Como base para a caracterização dos processos de interação de magmas, foram estimados os parâmetros físico-químicos dos magmas primários e híbridos identificados no plúton. As temperaturas liquidus foram estimadas a partir da saturação em apatita, e são da ordem de 950-1050°C para os magmas mais primitivos (Mdf) e 850-900°C para os mais diferenciados (quartzo sienitos). As temperaturas solidus, estimadas através das relações de equilíbrio entre hornblenda e plagioclásio, são da ordem de 750°C para Mdf, e 650-700°C para Sienitos e quartzo sienitos (Qsie). A profundidade de alojamento do plúton é estimada em ~13-15 km com base nas pressões estimadas para Mdf com base no conteúdo de Al na hornblenda. A concentração de H2O nos magmas foi estimada com base no teor de An do plagioclásio, conhecida a temperatura de cristalização, que indicou valores da ordem de 2,5-3,3% para Mdf, alcançando até 5% nos quartzo sienitos. Estimativas da fO2 a partir da composição química de cristais de magnetita e ilmenita não puderam ser obtidas, devido a reequilíbrio pós-magmático. Deste modo, foram obtidos valores aproximados com base no conteúdo de ulvoespinélio de cristais de magnetita reconstituídos e no conteúdo da molécula ilmenita dos cristais de ilmenita; em paralelo, foram também utilizadas as razões Fe/(Fe/Mg) de anfibólio e biotita. Os resultados revelaram um importante contraste entre as unidades Mdf e Mdr, caracteristicamente oxidadas, com valores próximos aos do buffer NNO, e as demais unidades, onde quartzo sienitos (Qsie) e especialmente Sie mostram-se mais reduzidas. Os baixos valores de susceptibilidade magnética medidos em campo para as unidade Sie e Mh, que a ela se associa, devem ser reflexos do seu caráter mais reduzido. Ao longo da história de construção da câmara, que foi alimentada intermitentemente por magmas de composição variada, dois eventos principais de interação de magmas foram identificados, com características distintas: (i) interação de magmas monzodioríticos (Mdf) e sieníticos (Sie), gerando a unidade de Monzonitos heterogêneos (Mh), na qual a intensa interdigitação de porções monzodioríticas e sieníticas sugere uma forte atuação mecânica, favorecendo a hipótese de que os magmas tenham se misturado previamente ao alojamento final; e (ii) interação de magmas monzodioríticos (Mdf) e quartzo sieníticos (Qsie), gerando diversas estruturas de coexistência, mistura localizada e possivelmente as rochas quartzo monzoníticas da unidade ( Qsie); neste caso, a interação entre os magmas possivelmente ocorreu na câmara magmática, como sugerido pelas características das estruturas indicativas de coexistência (enclaves e pillows de composição monzodiorítica).
The present study investigates the interaction and partial mixing of monzodiorite and syenite s.l. magmas in the Piracaia Pluton (~580 My), which is part of the post-orogenic Itu Granite Province. The Piracaia Pluton is an elongated intrusion with approximately 30 km², composed by five units: Coarse-grained monzodiorites (Mdr); Fine-grained monzodiorites (Mdf); Heterogeneous monzonites (Mh); Syenites (Sie); quartz syenites and quartz monzonites (Qsie). The physico-chemical crystallization parameters of the primary and hybrid magmas identified in the pluton were determined as references for the characterization of the magma interaction processes. The liquidus temperatures were estimated based on apatite saturation, and are in the range of 950-1050º C for the most primitive magmas (Mdf) and 850-900º C for the more differentiated ones (quartz syenites). The solidus temperatures, estimated on the basis of the equilibrium between hornblende and plagioclase, are about 750º C for Mdf, and 650-700º C for and quartz syenites (Qsie). The depth of emplacement is estimated at 13-15 km, as indicated by pressure estimates for Mdf, based on the Al-in-hornblende content. The H2O concentration of the magmas was estimated based on the An content of plagioclase, with results are in the range of 2.5-3.3% for Mdf, reaching up to 5% in quartz syenites. fO2 estimates based on the composition of coexisting magnetite and ilmenite could not be performed, due to post-magmatic re-equilibration. However, approximate values were obtained based on the ulvospinel content of reconstructed titanomagnetite crystals, and on the content of ilmenite molecule in ilmenite crystals; in parallel, the Fe/(Fe/Mg) ratios of amphibole and biotite were also used. The results show an important difference between the Mdf and Mdr units, which are distinctively oxidized, with values near the NNO buffer, and the other units which have lower ?O2, the quartz syenites and especially the syenites being the more reduced units. The lower magnetic susceptibility values measured in the field for the Sie and Mh units must reflect their more reduced nature. During the construction of the magma chamber, which was intermittently recharged by magmas of varied composition, two main events of magma interaction with distinct characteristics were identified: (i) the interaction of monzodiorites (Mdf) and syenites (Sie), generating the Heterogeneous monzonite unit, in which the interfingering of monzodiorite and syenite portions suggest a strong mechanical interaction, favoring the hypothesis that the magmas were already mixing previously to the final emplacement; (ii) interaction of monzodiorite (Mdf) and quartz syenite (Qsie), generating diverse mingling structures, local hybridization and possibly the quartz monzonite rocks of the unit Qsie; in this case, the magma interaction must have occurred at the magma chamber, as suggested by the type of structures indicative of coexistence (enclaves and monzodiorite pillows).
APA, Harvard, Vancouver, ISO, and other styles
7

Ryskamp, Elizabeth Balls. "Petrogenesis of Eocene-Oligocene magmatism of the Sulphur Springs Range, central Nevada: The role of magma mixing." Diss., CLICK HERE for online access, 2006. http://contentdm.lib.byu.edu/ETD/image/etd1607.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Le, Roux Véronique. "Interactions magma-roche et déformation en présence de magmas dans les péridotites de Lherz : implications pour l'évolution structurale, chimique et isotopique du manteau lithosphérique." Montpellier 2, 2008. http://www.theses.fr/2008MON20113.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Morgavi, Daniele. "Magma mixing." Diss., Ludwig-Maximilians-Universität München, 2014. http://nbn-resolving.de/urn:nbn:de:bvb:19-165555.

Full text
Abstract:
In order to increase our understanding of magma mixing processes and their impact on the geochemical evolution of silicate melt we present in the following works, the first set of experiments performed using natural basaltic and rhyolitic melts. In particular, we investigate the interplay of physical dynamics and chemical exchanges between these two melts using time-series mixing experiments performed under controlled, chaotic, dynamical conditions. The variation of major and trace elements is studied in detail by electron microprobe (EMPA) and Laser Ablation ICP-MS (LA-ICP-MS) and the time-evolution of chemical exchanges during mixing is investigated. Using the concentration variance as a proxy to measure the rate of chemical element homogenization in time, a model to quantify chemical element mobility during chaotic mixing of natural silicate melts is proposed. The morphology of mixing patterns at different times is quantified by measuring their fractal dimension and an empirical relationship between mixing time and morphological complexity is derived. The complexity of mixing patterns is also compared to the degree of homogenization of chemical elements during mixing and empirical relationships are established between the fractal dimension and the variation of concentration variance of chemical elements in time. Finally we discuss the petrological and volcanological implications of this work.
Um unser Verständnis über die Prozesse bei der Vermischung von Magmen und dessen Auswirkungen auf die geochemische Entwicklung von Silikatschmelzen zu verbessern, werden in dieser Arbeit erstmalig eine Reihe von „Magma Mixing“ Experimenten vorgestellt, in der natürliche Basalte und Rhyolite verwendet werden. In dynamischen Zeitreihen-Mischungsexperimenten, die unter kontrollierten, chaotischen, dynamischen, Bedingungen abliefen, wurde vor allem das Zusammenspiel der physikalischen Prozessen durch das mechanische Vermengen zweier Schmelzen und der resultierenden chemischen Austauschreaktionen durch Diffusion an den Grenzflächen zwischen diesen beiden Schmelzen untersucht. Die Variation von Haupt- und Spurenelementen wurde mittels Elektronen-Mikrosonde (EMPA) und Laser Ablation ICP-MS (LA-ICP-MS) im Detail untersucht und zusätzlich konnte die zeitliche Entwicklung des chemischen Austauschs während des Mischungsvorgang dargestellt werden. Die Varianz der Konzentration einzelner Elemente über die Grenzflächen zwischen Basalt und Rhyolit hinweg wurde als Proxy verwendet, um die Homogenisierungsrate der chemischen Elemente bezogen auf die Zeit zu bestimmen. Dies wird als Modell vorgeschlagen, mit dem die Mobilität chemischer Elemente während chaotischem Mischens von natürlichen Silikatschmelzen quantifiziert werden kann. Im Weiteren wurde mit Hilfe von Fraktalanalyse die Morphologie der Mischungsmustern zu unterschiedlichen Zeiten quantifiziert und eine empirische Beziehung zwischen Mischzeit und morphologischer Komplexität abgeleitet. Die Komplexität der Mischungsmuster wurde zudem mit dem Grad der Homogenisierung der chemischen Elemente während des Mischens verglichen. Dadurch konnten empirische Beziehungen zwischen der fraktalen Dimension von Mischungsmorphologien und der zeitlichen Variation der Konzentration von chemischen Elementen abgeleitet werden. Im Laufe dieser Arbeit werden zudem die petrologischen und vulkanologischen Auswirkungen diskutiert.
APA, Harvard, Vancouver, ISO, and other styles
10

Pommier, Anne. "Propriétés électriques des magmas." Phd thesis, Université d'Orléans, 2009. http://tel.archives-ouvertes.fr/tel-00545608.

Full text
Abstract:
Les expériences ont été menées pour déterminer les propriétés électriques des verres et liquides silicatés du Vésuve et du Kilauea par spectroscopie d'impédance. Une étude méthodologique des mesures à deux et quatre électrodes a amélioré la qualité des mesures électriques. Les mesures ont été faites entre 400 et 1400°C, 0.1 et 400MPa et pour des fugacités en oxygène de 10-8 à 0.2 bar. La conductivité électrique croît avec la température, les teneurs en eau et sodium et lorsque pression et fO2 diminuent. Des lois d'Arrhénius ont été déterminées dans les verres et liquides pour étudier les propriétés de transport. Des énergies d'activation de 60 à 150kJ/mol et un volume d'activation de 20cm3/mol ont été calculés. Une méthode semiempirique a été déduite pour estimer la conductivité d'une large gamme de melts. Une application géophysique de nos résultats a consisté en un modèle direct de la conductivité du Vésuve. Les fonctions de transfert s'expliquent par la seule présence d'une saumure. Sa forte conductivité rend la détection d'un corps magmatique profond difficile. Cependant, nos simulations ont démontré que les données géophysiques actuelles sont en accord avec un réservoir de magma cristallisé ou du magma plus chaud interconnecté dans l'encaissant carbonaté. Une application géochimique a consisté au suivi en temps réel des cinétiques redox dans des basaltes, en utilisant la dépendance au temps de la conductivité suite à un changement de fO2. L'évolution de la conductivité au cours du temps, liée à la mobilité du sodium, est identique à celle du ratio fer ferrique/fer ferreux du melt. La réduction sous CO-CO2 et l'oxydation à l'air sont limitées par la diffusion, mais pas l'oxydation sous CO2, probablement à cause de réactions à l'interface gaz/melt. Les valeurs calculées élevées de diffusivité et d'énergie d'activation ont été expliquées par des mécanismes redox impliquant une coopération entre flux d'alcalins, de cations divalents et d'oxygène.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Books on the topic "Magmax"

1

Middlemost, Eric A. K. Magmas, rocks and planetary development: A survey of magma/igneous rock systems. Harlow: Longman, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Astaloș, George. Magma. Bucharest: Vitruviu Pub. House, 1998.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Rosa, João Guimarães. Magma. Rio de Janeiro, RJ, Brasil: Editora Nova Fronteira, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Astaloș, George. Magma. Bucharest: Vitruviu Pub. House, 1998.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Biasiucci, Antonio. Magma. [Milano]: F. Motta, 1998.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Sinit︠s︡yn, Oleg. Magma: Roman. Moskva: Armada, 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Adami, Massimiliano. Magma fossile. Milano: La Triennale di Milano, Design Museum, 2009.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

Desfossés, Jacques. Magma: Roman. Montréal, Québec: Triptyque, 2000.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

Orlik, Piotr. Magma uczuć. Poznań: Wydawnictwo Naukowe Instytutu Filozofii Uniwersytetu im. Adama Mickiewicza, 2005.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Knežević, Rajko. Deca sunca: Magma. Beograd: V. Knežević, 2005.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Magmax"

1

Perugini, Diego. "The Beginning: Mafic Magmas Invading Felsic Magma Chambers." In The Mixing of Magmas, 77–86. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-81811-1_6.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Soreanu, Raluca. "Magmas." In Working-through Collective Wounds, 51–82. London: Palgrave Macmillan UK, 2018. http://dx.doi.org/10.1057/978-1-137-58523-3_3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Arndt, Nicholas. "Magma." In Encyclopedia of Astrobiology, 1413. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_915.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Schmincke, Hans-Ulrich. "Magma." In Volcanism, 21–34. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Arndt, Nicholas. "Magma." In Encyclopedia of Astrobiology, 1. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_915-3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Arndt, Nicholas. "Magma." In Encyclopedia of Astrobiology, 938. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_915.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Hickson, Catherine J., T. C. Spurgeon, and R. I. Tilling. "Magma." In Encyclopedia of Natural Hazards, 639–40. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-1-4020-4399-4_224.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Dobran, Flavio. "Magma Chambers." In Volcanic Processes, 327–410. Boston, MA: Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_5.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Maaløe, Sven. "Magma Kinetics." In Principles of Igneous Petrology, 230–88. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-49354-6_11.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Maaløe, Sven. "Magma Dynamics." In Principles of Igneous Petrology, 289–328. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-49354-6_12.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Magmax"

1

Wizenty, Philip, Jonas Sorgalla, Florian Rademacher, and Sabine Sachweh. "MAGMA." In ECSA '17: 11th European Conference on Software Architecture. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3129790.3129821.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Zokaee, Farzaneh, Mingzhe Zhang, Xiaochun Ye, Dongrui Fan, and Lei Jiang. "Magma." In DAC '19: The 56th Annual Design Automation Conference 2019. New York, NY, USA: ACM, 2019. http://dx.doi.org/10.1145/3316781.3317858.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Ichihara, Mie, Daniel Rittel, and M. B. Rubin. "Deformation and Fracture of a Silicate Melt Around Tg: Implications to Dynamics of Volcanic Eruptions." In ASME 2008 9th Biennial Conference on Engineering Systems Design and Analysis. ASMEDC, 2008. http://dx.doi.org/10.1115/esda2008-59494.

Full text
Abstract:
The mechanical properties of magma around the glass transition temperature have not been characterized yet, though this subject is considered to be important in dynamics of volcanic eruptions. In this paper, we present an experimental investigation of stress-strain relation of synthetic magma at various temperatures and strain rates. The material behaves as an elastic solid at low temperature and/or high strain rate, and as a viscous fluid at high temperature and/or low strain rate. In the transition, it reveals work-hardening response. Although the work-hardening nature has not been reported for noncrystalline magma, it is important in constructing a mathematical model to represent the flow-to-fracture transition of magma, namely the transition of eruptions from effusive to explosive styles.
APA, Harvard, Vancouver, ISO, and other styles
4

Horváth, Györgyi, Kamilla Ács, Viktória Lilla Balázs, Eszter Csikós, Amir Reza Ashraf, Béla Kocsis, Andrea Böszörményi, et al. "A fahéjkéreg-illóolaj alkalmazhatósága légúti betegségek esetén – pécsi tapasztalatok." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.a1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Horányi, Tamás. "A tudomány és a szabályozás „konfliktusa”:." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.a2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Vasas, Andrea, Csaba Bús, Dóra Stefkó, Norbert Kúsz, Barbara Tóth, and Judit Hohmann. "Juncaceae fajok, mint ígéretes fenantrénforrások." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.a3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Vasas, Gábor, József Deli, Milán Riba, Andrea Ujvárosi, Martin Hanyicska, Sándor Gonda, and Kitti Kapás. "Karotinoid- és peptidmintázatok elemzése mikroalgákból." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.a4.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Tóth, Barbara, Tamás Lantos, Péter Hegyi, Réka Viola, and Dezső Csupor. "A gyömbér posztoperatív hányinger- és hányáscsillapító hatásának metaanalízise." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.b1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Pluhár, Zsuzsanna, Szilvia Tavaszi-Sárosi, Enikő Détár, Éva Zámboriné Németh, Dóra Szabó, and Katarzyna Seidler-Łożykowska. "A kerti kakukkfű (Thymus vulgaris L.) fajták illóolaj-jellemzőit befolyásoló tényezők értékelése." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.b2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Bérci, István. "Gyógynövény készítmények kockázatértékelése a „Biztonságos étrend-kiegészítő program” keretében." In XV. Magyar Gyógynövény Konferencia. Szeged: Magyar Gyógyszerésztudományi Társaság Gyógynövény Szakosztálya, 2018. http://dx.doi.org/10.14232/mgyk.2018.b3.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Magmax"

1

Hollander, Attelia. Diagnostic Testing for COVID-19 Bridging Study for QIAamp Viral RNA Extraction vs Beckman RNAdvance vs Thermofisher MagMAX. Office of Scientific and Technical Information (OSTI), February 2021. http://dx.doi.org/10.2172/1766984.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

D. Krier. Magma Dynamics at Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), August 2005. http://dx.doi.org/10.2172/859089.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Dunn, J. C., ed. Magma energy extraction - Annual Report for FY88. Office of Scientific and Technical Information (OSTI), August 1989. http://dx.doi.org/10.2172/5499960.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Wemple, R. P., and D. B. Longcope. Thermal stress fracturing of magma simulant materials. Office of Scientific and Technical Information (OSTI), October 1986. http://dx.doi.org/10.2172/7049178.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Baryshkov, D. GOST R 34.12-2015: Block Cipher "Magma". Edited by V. Dolmatov. RFC Editor, September 2020. http://dx.doi.org/10.17487/rfc8891.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Grondahl, C., A. Tsay, and Z. Zajacz. Controls on the ore fertility of arc magmas. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/315007.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

B. Damjanac and E.S. Gaffney. CONDITIONS LEADING TO SUDDEN RELEASE OF MAGMA PRESSURE. Office of Scientific and Technical Information (OSTI), August 2005. http://dx.doi.org/10.2172/884943.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Carson, C. C. Selection of promising sites for magma energy experiments. Office of Scientific and Technical Information (OSTI), January 1985. http://dx.doi.org/10.2172/6143303.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Cameron, E. M., and W. J. Carrigan. Oxygen Fugacity of Archean Felsic Magmas: Relationship To Gold Mineralization. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122478.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Kukacka, L. E. Tapping the earth's geothermal resources: Hydrothermal today, magma tomorrow. Office of Scientific and Technical Information (OSTI), December 1986. http://dx.doi.org/10.2172/6147714.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Magmax' for particular source types:
Journal articles Dissertations / Theses Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography