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high magnesian

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Journal Article
Journal: GSA Bulletin
Published: 01 October 1965
GSA Bulletin (1965) 76 (10): 1191–1196.
...GERALD M FRIEDMAN Abstract A relationship exists between the mineralogy and the environment of deposition of Recent carbonate sediments; deep-sea carbonate sediments contain abundant low-magnesian calcite, whereas shallow-water sediments are high in high-magnesian calcite and aragonite...
Journal Article
Published: 01 February 2018
American Mineralogist (2018) 103 (2): 216–240.
.... 1999 ; Greene et al. 2006 ; Horodyskyj et al. 2009 ). We predict that such melts could be moderately water-rich (if formed at sufficiently high pressure, say in the deep crust), highly magnesian, and could mix with the intrusive magma to produce PBA-like liquids that, in turn, could be trapped...
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Journal Article
Journal: Geology
Published: 01 April 2007
Geology (2007) 35 (4): 351–354.
... generally recognized, and that their magnesian compositions do not necessarily imply that they are primitive mantle melts. 27 11 2006 11 08 2006 22 11 2006 Geological Society of America 2007 high-magnesian andesite primitive magnesian andesite Mount Shasta mixing adakite arc...
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Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): e147.
..., Yb, Pb, and Zr. This illustrates the inability of the mixing models to produce the HMA with any third component, Trinity ophiolite or otherwise. Figure 1 Predicted isotopic composition of the Mt. Shasta high-magnesian andesite (HMA), using the mixing models of Streck et al. (2007) , are shown...
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Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): e148.
.... 37 , p . 530 – 552 , doi: 10.1007/BF02596890 . Barr J. Grove T.L. Elkins-Tanton L. 2007 , High-magnesian andesite from Mount Shasta: A product of magma mixing and contaminations, not a primitive melt: Comment : Geology , doi: 10.1130/G24058C.1 . Borg L.E. Brandon...
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Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): e149–e150.
.... Chesley J. 2007 , High-magnesian andesite from Mount Shasta: A product of magma mixing and contamination, not a primitive mantle melt : Geology , v. 35 , p . 351 – 354 , doi: 10.1130/G23286A.1 . Yogodzinski G.M. Kelemen P.B. 1998 , Slab melting in the Aleutians: Implications...
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Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): e150.
.... 148 , p . 542 – 565 , doi: 10.1007/s00410-004-0619-6 . Kelemen P.B. Yogodzinski 2007 , High-magnesian andesite from Mount Shasta: A product of contamination, not primitive melt: Comment : Geology , doi: 10.1130/G24099C.1 . Kelemen P.B. Hanghoj K. Greene A.R. 2003...
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Journal Article
Published: 01 June 1999
Jour. Geol. Soc. India (1999) 53 (6): 693–704.
...Rajesh K. Srivastava; R. K. Singh Abstract Greenschist facies rnetabasalts showing relict spinifex texture, associated with the Late Archaean Bengpal Group, are well exposed in the Kaklur area, Bastar craton. They are classified as siliceous high-magnesian basalts (SHMB) on the basis of its...
Journal Article
Published: 01 April 1998
Journal of the Geological Society (1998) 155 (2): 269–280.
... representing high-magnesian andesites.Sr and Nd isotopic data indicate that the andesites range isotopically to more depleted mantle compositions than the associated basalts. The dacite/rhyolites can be related compositionally to the andesites by assimilation of typical Pacific rim accretionary material...
Journal Article
Journal: Geology
Published: 01 January 1997
Geology (1997) 25 (1): 42–44.
... above 1100 °C have basaltic compositions. This suggests that high-magnesian andesites can be formed by direct partial melting of the hydrous upper mantle only at relatively low temperatures. These andesitic melts, together with those obtained at 1100 °C, contain more than 3 wt% H 2 O and have...
Journal Article
Published: 01 December 1976
Journal of Sedimentary Research (1976) 46 (4): 940–951.
... to sediment bodies of accumulated shell material mixed with quartz sand and 2) cement of magnesian calcite associated with sediment bodies of almost pure quartz sand. Both types of cement are present at all localities studied. The magnesian calcite shows a variable magnesium content in the range of 10-25 wt...
Journal Article
Published: 01 January 2010
American Mineralogist (2010) 95 (1): 177–184.
... 13 950 145 Au-Pd Spr, Crn, Hem, Melt 12 08 2009 16 12 2008 © 2010 American Mineralogist 2010 High P-T experiment magnesian staurolite ultrahigh-temperature (UHT) metamorphism Southern Indian Granulite Terrane Limpopo Belt (southern Africa) Moderate-Mg...
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Journal Article
Published: 01 November 1985
The Canadian Mineralogist (1985) 23 (4): 609–618.
Image
Predicted isotopic composition of the Mt. Shasta high-magnesian andesite (HMA), using the mixing models of Streck et al. (2007), are shown as Model 1 and Model 2. Trinity ophiolite samples (including two that plot outside of the region shown—indicated by arrows) from Jacobsen et al. (1984) and Gruau et al. (1995). Dacite (83–58), HAOT (85–38), CAB (85–1a), and HMA (85–41b) samples are all from Grove et al. (2002). Mt. Lassen HMA (LC86–1009) is from Borg et al. (1997). CAB—calc-alkaline basalt; HAOT—high-alumina olivine tholeiite.
Published: 01 January 2007
Figure 1 Predicted isotopic composition of the Mt. Shasta high-magnesian andesite (HMA), using the mixing models of Streck et al. (2007) , are shown as Model 1 and Model 2. Trinity ophiolite samples (including two that plot outside of the region shown—indicated by arrows) from Jacobsen et al
Image
Mt. Shasta lavas compared to Aleutian high-magnesian andesite (A-HMA) (data sources and legend as in Fig, 1 and Grove et al. [2002]). Double-headed arrow defines trend in Mt. Shasta dacites (62–64 wt% SiO2).
Published: 01 January 2007
Figure 2 Mt. Shasta lavas compared to Aleutian high-magnesian andesite (A-HMA) (data sources and legend as in Fig, 1 and Grove et al. [2002]). Double-headed arrow defines trend in Mt. Shasta dacites (62–64 wt% SiO 2 ).
Image
Diagram fO2 – T (A) and Pl–Ol–Q (B) for high-magnesian (HMA), high-phosphorous (HPA), high-(HKA), medium-(MKA) and low-potassium (LKA) andesites as well as for andesites of the Aukan volcanic center (A). Figure A shows the positions of standard hematite–magnetite (HM) and quartz-fayalite-magnetite (QFM) buffers. Figure B shows the location of experimentally obtained cotectic for 1 atm, 8 kbar (“dry” system) and 5 kbar at 2 % H2O.
Published: 01 November 1996
Fig. 3. Diagram f O 2 – T ( A ) and Pl–Ol–Q ( B ) for high-magnesian (HMA), high-phosphorous (HPA), high-(HKA), medium-(MKA) and low-potassium (LKA) andesites as well as for andesites of the Aukan volcanic center ( A ). Figure A shows the positions of standard hematite–magnetite (HM
Image
—Scanning electron micrograph of cryptocrystalline high-magnesian calcite cement in grapestone.
Published: 01 March 1973
Fig. 17. —Scanning electron micrograph of cryptocrystalline high-magnesian calcite cement in grapestone.
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1973
AAPG Bulletin (1973) 57 (3): 541–557.
...Fig. 17. —Scanning electron micrograph of cryptocrystalline high-magnesian calcite cement in grapestone. ...
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Journal Article
Published: 01 May 1991
Journal of Sedimentary Research (1991) 61 (3): 364–369.
... originally composed of high-magnesian calcite. The delicate reticulate structure of pillars and growth laminations of the original stromatoporoid coenosteum is represented by a neomorphic fabric of microdolomite-rich zones of inclusions in low-magnesian calcite. In comparison, co-existing constituents...
Journal Article
Journal: Geosphere
Published: 26 May 2020
Geosphere (2020) 16 (4): 1012–1041.
... of California (<12 Ma). In addition, a suite of postsubduction rocks (<12 Ma), referred to as “bajaites,” are enriched in light rare-earth and other incompatible elements (e.g., Ba and Sr). These are further subdivided into high-magnesian andesite (with 50%–58% SiO 2 and MgO >4%) and adakite (>56...
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