Jorullo Volcano, Michoacan, Mexico: the earliest stages of fractionation in calc-alkaline magmas
Between 1759 and 1774, Jorullo Volcano and four associated cinder cones erupted approximately 2 km/sup 3/ of magma which evolved progressively with time from early ol-hy-normative primitive basalts (Mgnumber=73, 516 ppm Cr, 260 ppm Ni) to late-stage qtz-hy-normative basaltic andesites. All lavas contain <6 vol% phenocrysts of magnesian olivine (fO/sub 90-70/) with Cr-Al-Mg spinel inclusions, and microphenocrysts of plagioclase and augite. Smooth whole-rock major and trace element compositional trends through the suite can be largely modeled by simple crystal fractionation of olivine, augite, plagioclase, and minor spinel. In order for augite and plagioclase to have been near-liquidus phases, the modeled crystal fractionation event must have occurred at lower-crustal to upper-mantle pressures (8-15 Kb). The crystals actually present in the Jorullo lavas, however, formed at low pressures. Compared to modeled abundances, La, Ce, Rb, Sr, Ba, Hf, Th, and Ta are anomalously enriched in the late-stage basaltic andesites and Dy, Yb, and Lu are anomalously depleted. These discrepancies apparently indicate the importance of other magma-chamber processes. Most high-alumina basalts reported in the literature have 18 to 21 wt% Al/sub 2/O/sub 3/, but are too depleted in MgO, Cr, and Ni to be direct mantle products. These high-alumina basalts have probably undergone significant fractionation of olivine, augite, plagioclase, and spinel from primitive parental basalt similar to the early Jorullo magmas. For hydraulic reasons, such primitive basalts are rarely erupted in mature arcs, and may be completely absent from mature stratovolcanoes.
- Research Organization:
- Franklin and Marshall College, Lancaster, PA (USA)
- OSTI ID:
- 6453125
- Report Number(s):
- CONF-8510489-
- Journal Information:
- Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
- Country of Publication:
- United States
- Language:
- English
Similar Records
Eruptive Activity on the Western Flank of Piton de la Fournaise (La RĂ©union Island, Indian Ocean): Insights on Magma Transfer, Storage and Evolution at an Oceanic Volcanic Island
Minettes and related lavas near Mascota, Jalisco, Mexico
Related Subjects
ANDESITES
CHEMICAL COMPOSITION
MINERALOGY
PETROGENESIS
BASALT
MEXICO
ERUPTION
FELDSPARS
FRACTIONATION
INCLUSIONS
LAVA
MAGMATISM
OLIVINE
PETROCHEMISTRY
SPINELS
VOLCANISM
VOLCANOES
ALKALINE EARTH METAL COMPOUNDS
ALUMINIUM COMPOUNDS
ALUMINIUM OXIDES
CHALCOGENIDES
DEVELOPING COUNTRIES
IGNEOUS ROCKS
IRON COMPOUNDS
IRON SILICATES
LATIN AMERICA
MAGNESIUM COMPOUNDS
MAGNESIUM OXIDES
MAGNESIUM SILICATES
MINERALS
NORTH AMERICA
OXIDE MINERALS
OXIDES
OXYGEN COMPOUNDS
ROCKS
SEPARATION PROCESSES
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
TRANSITION ELEMENT COMPOUNDS
VOLCANIC ROCKS
580400* - Geochemistry- (-1989)
580300 - Mineralogy
Petrology
& Rock Mechanics- (-1989)