22 research outputs found
Crustal Forensics in Arc Magmas
Abstract The geochemical characteristics of continental crust are present in nearly all arc magmas. These characteristics may reflect a specific source process, such as fluid fluxing, common to both arc magmas and the continental crust, and/or may reflect the incorporation of continental crust into arc magmas either at source via subducted sediment, or via contamination during differentiation. Resolving the relative mass contributions of juvenile, mantle-derived material, versus that derived from pre-existing crust of the upper plate, and providing these estimates on an element-by-element basis, is important because: (1) we want to constrain crustal growth rates; (2) we want to quantitatively track element cycling at convergent margins; and (3) we want to determine the origin of economically important elements and compounds. Traditional geochemical approaches for determining the contributions of various components to arc magmas are particularly successful when applied on a comparative basis. Studies of suites from multiple magmatic systems along arcs, for which differentiation effects can be individually constrained, can be used to extrapolate to potential source compositions. In the Lesser Antilles Arc, for example, differentiation trends from individual volcanoes are consistent with open-system evolution. However, such trends do not project back to a common primitive magma composition, suggesting that differentiation modifies magmas that were derived from distinct mantle sources. We propose that such approaches should now be complemented by petrographically constrained mineral-scale isotope and trace element analysis to unravel the contributing components to arc magmas. This innovative approach can: (1) better constrain true end-member compositions by returning wider ranges in geochemical compositions among constituent minerals than is found in whole rocks; (2) better determine magmatic evolution processes from core–rim isotopic or trace element profiles from the phases contained in magmas; and (3) constrain rates of differentiation by applying diffusion-controlled timescales to element profiles. An example from Nguaruhoe Volcano, New Zealand, underscores the importance of such a microsampling approach, showing that mineral isotopic compositions encompass wide ranges, that whole-rock isotopic compositions are consequently simply element-weighted averages of the heterogeneous crystal cargo, and that open-system evolution is proved by core–rim variations in Sr isotope ratios. Nguaruhoe is just one of many systems examined through microanalytical approaches. The overwhelming conclusion of these studies is that crystal cargoes are not truly phenocrystic, but are inherited from various sources. The implication of this realization is that the interpretation of whole-rock isotopic data, including the currently popular U-series, needs careful evaluation in the context of petrographic observations
Mineral inventory of continuously erupting basaltic andesites at Arenal volcano, Costa Rica: implications for interpreting monotonous, crystal-rich, mafic arc stratigraphies
Except for the first 2 years since July 29, 1968, Arenal volcano has
continuously erupted compositionally monotonous and phenocryst-rich
(similar to35%) basaltic andesites composed of plagioclase (plag),
orthopyroxene (opx), clinopyroxene (cpx), spinel olivine. Detailed
textural and compositional analyses of phenocrysts, mineral inclusions,
and microlites reveal comparable complexities in any given sample and
identify mineral components that require a minimum of four
crystallization environments. We suggest three distinct crystallization
environments crystallized low Mg# (<78) silicate phases from andesitic
magma but at different physical conditions, such as variable pressure of
crystallization and water conditions. The dominant environment, i.e.,
the one which accounts for the majority of minerals and overprinted all
other assemblages near rims of phenocrysts, cocrystallized clinopyroxene
(Mg# similar to71-78), orthopyroxene (Mg# similar to71-78),
titanomagnetite and plagioclase (An(60) to An(85)). The second
environment cocrystallized clinopyroxene (Mg# 71-78), olivine
(<Fo(78)), titanomagnetite, and very high An (similar to90) plagioclase,
while the third cocrystallized clinopyroxene (Mg# 71-78) with high (>7)
Al/Ti and high (>4 wt.%) Al2O3, titanomagnetite with considerable Al2O3
(10-18 wt.%) and possibly olivine but appears to lack plagioclase. A
fourth crystallization environment is characterized by clinopyroxene
(e.g., Mg#=similar to78-85; Cr2O3=0.15-0.7 wt.%), Al-, Cr-rich spinel
olivine (similar toFo(80)), and in some circumstances high-An (>80)
plagioclase. This assemblage seems to record mafic inputs into the
Arenal system and crystallization at high to low pressures.
Single crystals cannot be completely classified as xenocrysts,
antecrysts (cognate crystals), or phenocrysts, because they often
contain different parts each representing a different crystallization
environment and thus belong to different categories. Bulk compositions
are mostly too mafic to have crystallized the bulk of ferromagnesian
minerals and thus likely do not represent liquid compositions. On the
other hand, they are the cumulative products of multiple mixing events
assembling melts and minerals from a variety of sources. The driving
force for this multistage mixing evolution to generate erupting basaltic
andesites is thought to be the ascent of mafic magma from lower crustal
levels to subvolcanic depths which at the same time may also go through
compositional modification by fractionation and assimilation of country
rocks. Thus, mafic magmas become basaltic andesite through mixing,
fractionation and assimilation by the time they arrive at subvolcanic
depths. We infer new increments of basaltic andesite are supplied nearly
continuously to the subvolcanic reservoir concurrently to the current
eruption and that these new increments are blended into the residing,
subvolcanic magma. Thus, the compositional monotony is mostly the
product of repetitious production of very similar basaltic andesite.
Furthermore, we propose that this quasi-constant supply of small
increments of magma is the fundamental cause for small-scale,
decade-long continuous volcanic activity; that is, the current eruption
of Arenal is flux-controlled by inputs of mantle magmas. (C) 2004
Elsevier B.V. All rights reserved
The role of basalt replenishment in the generation of basaltic andesites of the ongoing activity at Arenal volcano, Costa Rica: evidence from clinopyroxene and spinel
The bulk composition of magma erupted from Volcan Arenal has remained
nearly constant (SiO2 = 53.6-54.9 wt%; MgO = 5.0-4.5 wt%) during
almost 30 years of continuous activity (1969-1996). None the less,
clinopyroxene (cpx) phenocrysts and their spinel inclusions record a
much more complex open-system evolution in which steady-state production
of the erupted basaltic andesitic magma is linked to episodic injections
of basalt into Arenal's magma conduit/reservoir system. High-resolution
major element zoning profiles (electron microprobe) on a large number of
phenocrysts (>14,000 analyses), tied to back-scattered electron (BSE)
images, have been used to assess the compositional characteristics of
the magmatic end members as well as the timing and dynamics of magma
replenishment events. No two cpx phenocrysts have exactly the same
zoning profile. The vast majority of our analyses record the
crystallization of cpx (Cr2O3 < 0.12 wt%; Mg# = 65-79; Al/Ti = 2-7)
from a liquid comparable to or more evolved than erupted magma
compositions. However, half of all cpx grains are cored by high-Cr cpx
(Cr2O3 = 0.2-0.72 wt%) or contain similar basaltic compositions as
abrupt growth bands in phenocrysts with and without high-Cr cores;
phenocrysts with high-Cr cpx occur throughout the ongoing activity. In a
few cases, high-Cr cpx occurs very near the outer margin of the grain
without an apparent growth hiatus, particularly in 1968/69 and 1992/93.
The main conclusions are: (1) all basaltic andesitic lavas erupted at
Arenal during the ongoing activity that began in July, 1968, are the
products of magma mixing, (2) clinopyroxenes record multiple
replenishment events of basaltic magma in contrast to the near constancy
of erupted bulk compositions, (3) some phenocrysts preserve records of
multiple interactions with basaltic magmas requiring magmatic processes
to operate on time-scales shorter than residence times of some
phenocrysts, (4) multiple occurrences of clinopyroxene with high-Cr rims
suggest that basalt replenishment events have occurred with sub-decadal
frequency and may predate eruption by months or less. From this we infer
that Arenal volcano is underlain by a continuously active, small-volume
magmatic reservoir maintained in quasi-steady state by basalt recharge
over several decades. The monotony of erupting Arenal magmas implies
that fractionation, recharge, ascent, and eruption are well balanced in
order for magmas to be essentially uniform while containing phenocrysts
with vastly different growth histories at the time of eruption
How do olivines record magmatic events? Insights from major and trace element zoning
Reconciling the diverse records of magmatic events preserved by multiple crystals and minerals in the same sample is often challenging. In the case of basaltic–andesites from Volcán Llaima (Chile), Mg zoning in olivine is always simpler than Ca zoning in plagioclase. A model that explains a number of chemical patterns is that Llaima magmas stall in the upper crust, where they undergo decompression crystallization and form crystal-mush bodies. Frequent magma inputs from deeper reservoirs provide the potential for remobilization and eruption. The records of multiple recharge events in Llaima plagioclase versus an apparent maximum of one such event in coexisting olivine are addressed by using trace element zoning in olivine phenocrysts. We have integrated elements that (1) respond to changes in magma composition due to recharge or mixing (Mg, Fe, Ni, Mn, ±Ca), with (2) elements that are incorporated during rapid, disequilibrium crystal growth (P, Ti, Sc, V, Al). A more complex history is obtained when these elements are evaluated considering their partition coefficients, diffusivities, and crystal growth rates. The olivine archive can then be reconciled with the plagioclase archive of magma reservoir processes. Olivine (and plagioclase) phenocrysts may experience up to three or more recharge events between nucleation and eruption. Diffusion modeling of major and trace element zoning in two dimensions using a new lattice Boltzmann model suggests that recharge events occur on the order of months to a couple of years prior to eruption, whereas crystal residence times are more likely to be on the order of a few years to decades.NRF (Natl Research Foundation, S’pore)MOE (Min. of Education, S’pore)Published versio
Tracking the evolution of large-volume silicic magma reservoirs from assembly to supereruption
Please help populate SUNScholar with the full text of SU research output. Also - should you need this item urgently, please send us the details and we will try to get hold of the full text as quick possible. E-mail to [email protected]. Thank you.Journal Articles (subsidised)NatuurwetenskappeAardwetenskapp
Recommended from our members
Assimilation of the Plutonic Roots of the Andean Arc Controls Variations in U-series Disequilibria at Volcan Llaima, Chile
U-series disequilibria provide important constraints on the processes and time scales of melt production, differentiation, and transport in subduction settings. Such constraints, which are essential for understanding the chemical evolution of the continental crust, are conventionally based on the assumption that the U-series disequilibria measured in mafic lavas are produced during mantle metasomatism and melting, and that intracrustal differentiation and assimilation have limited impacts. Here we show that mantle-derived U-series disequilibria in mafic lavas erupted at Volcán Llaima, Chile are significantly diminished by assimilation of plutonic rocks forming Llaima's subvolcanic basement. This contamination process is extremely subtle in terms of “classical” indicators of crustal assimilation like Sr, Nd or Pb isotopes because it is a manifestation of assimilative recycling of the plutonic roots of the arc. This process results in variations in U-series disequilibria and incompatible trace element ratios that are significant compared to regional and global variability in arc magmas. Furthermore, it yields linear correlations between U-series excesses and incompatible trace element ratios that are generally interpreted as slab-fluid indicators and chronometers, or tracers of sediment recycling in subduction zone. Cannibalization of ancestral magmas by ascending melts warrants careful evaluation when considering the components and chemical fluxes in subduction zones. Linear arrays defined by activity ratios of U-series nuclides with different half-lives may be the most reliable indicators of assimilative recycling of ancestral intrusive magmas.Earth and Planetary Science