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Returning to Keiko Hattori’s Home page
Arc volcanoes discharge large quantities of
H2O, CO2 and SO2. Some volcanoes
discharge huge SO2, some are not. Some arcs are very fertile in base
metals, producing many metallic deposits.
I am interested in understanding the reasons why some arcs are very
fertile, how metallic elements are transferred from subducting
slabs to arc magmas via sub-arc mantle (i.e., element recycling), how volatile
elements are subducted and moved to the interior of
mantle wedges where arc magmas are generated..
To understand the processes and paths, I
examine forearc mantle peridotites
(serpentinites, xenoliths) and primitive arc magmas.
The research involves the following areas
of study.
Study 1. Study of forearc mantle peridotites (Himalayas, Alps, Cuba, Dominican Republic,
Japan).
Serpentin is stable down to a depth of ~ 130 km and contain high contents of
water (up to 17 wt%).
Therefore, serpentin is a reservoir of water and
fluid-mobile elements in the mantle. A layer of serpentinites
forms at the base of mantle wedges as subducting
slabs release water and fluid-mobile elements,, such
as arsenic, antimony, strontium and lead. The serpentinites
are dragged down to deep levels by mantle corner flow and eventually dehydrated
back to anhydrous phases. The dehydration of forearc
mantle serpentinites discharges water to the interior
of mantle wedges, which results in partial melting of arc magmas.
Study 2. Composition of primitive arc magmas
and subarc mantle
The composition
of subarc mantle is studied using primitive arc
magmas and xenoliths that were brought up to the surface by explosive arc
igneous rocks.
Cees Jan de Hoog carried out a study, primitive mafic magmas at
Jian Wang
studied the compositions of subarc mantle as his PhD
thesis project. His work has been
published in Contributions to Mineralogy and Petrology, Lithos and
Mineralogy and Petrology. He is
currently Professor at
Study of forearc mantle
Stern,
F.J., Hattori, K.H., 2011. Mantle evolution recorded in Cr-spinel from the Bay of Island Ophiolitic
Complex, Northern Appalachians. Abst. Geological Society of America Annual
Meeting. Vol. 43, no. 5. p..493.
pdf file
Saumur, B.M., Hattori, K.H., Stern F.,
and Jackson, S., 2011. Major and trace element compositions
of Cr-spinel from serpentinized
forearc mantle peridotites:
insights on their behavior during melt extraction and
metamorphism. Abst. Geological Society of America Annual
Meeting. Vol. 43, no. 5. p..588.
pdf
file
Deschamps,
F., Guillot, S., Godard, M., Andreani, M., Hattori, K., 2011. Serpentinites acting as a
sponge for fluid-mobile elements in abyssal peridotites, Terra Nova. V. 23, p.
171-178. doi: 10.1111/j.1365-3121.2011.00995.x, pdf file
De Hoog, JCM, Janák,M., Vrabec,M., Hattori, KH., 2011, Ultramafic cumulates of oceanic
affinity in an intracontinental subduction
zone: ultrahigh-pressure garnet peridotites from Pohorje (Eastern Alps, Slovenia). In “Ultrahigh pressure metamorphism:
25 years after first discovery of coesite and diamond”
Eds. L. Dobrzhinetskaya, S. Cuthbert and W. Faryad, Elsevier Publ., DOI:
10.1016/B978-0-12-385144-4.00012-6. pdf
file
Hattori,
K., Guillot, S., Saumur, BM, Tubrett, M.N., Vidal, O., Morfin,
S., 2010. Corundum-bearing
garnet peridotites from northern
Hattori, K., Wallis, S., Enami,
T. and Mizukami, T., 2010, Subduction of mantle wedge peridotites:
Evidence from the Higashi-akaishi ultramafic
body in the Sanbagawa metamorphic belt. Island Arc. Vol. 19, p.192-207. Pdf file
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Higashi-akaishi body is mostly dunite (not hydrated) and minor intercalating garnet clinopyroxenite (again not hydrated). |
chromitite
seams in dunite |
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Surrounding eclogite
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Deschamps, F., Guillot, S., Godard, M., Chauvel, C. Andreani, M.,
Hattori, K., 2010. In
situ characterization of serpentinites from hydrated forearc mantle wedge: Timing of serpentinization
and fluid mobile elements behaviour in subduction
zones. Chemical Geology. vol.
269, p. 262-277 abstract, full pdf
Saumur, B-M, Hattori, K.,
Guillot, S., 2009, Constrasting
origins of serpentinites in a subduction
complex, northern Dominican Republic. Geological Society of America Bulletin. vol.
122, p. 292-304. with Data Repository 2009134.
Guillot, S., Hattori, K., Schwartz, S. and Vidal,
O., 2009, Exhumation processes in oceanic and continental contexts: High
pressure and ultrahigh pressure rocks” In (edited by S. Lallemand
& F. Funiciello) Subduction Zone Geodynamics (doi; 10.1007/978-3-540-87974-9), p.175-205.
pdf file (13 Mb)
Wang, J.,Hattori,
K.H., Stern, C., 2008, Metasomatic
origin of garnet orthopyroxenites in the subcontinental lithospheric
mantle underlying Pali Aike
volcanic field, southern
Wang,
J., Hattori, K.H., Li, J-P, Stern,C.R.,
2008, Oxidation state of Paleozoic subcontinental lithospheric
mantle below the Pali Aike
volcanic field in southernmost
Guillot, S., Mahéo, G., de Sigoyer, J.,
Hattori, K., Pêcher, A., 2008, Tethyan
and Indian subduction viewed from the Himalayan high-
to ultrahigh- pressure metamorphic rocks. Tectonophysics,
10.1016/j.tecto.2007.11.059 pdf file (2.3 Mb)
Morishita, T., Hattori,
K., Terada, K., Matsumoto, T., Yamamoto, K., Arai, S., 2008. Geochemical investigations on apatite-rich
layers in the Finero phlogopite-peridotite
massif (Italian Western Alps) and ion microprobe dating of apatite. Chemical
Geology vol.
251, p. 99-111 pdf file
Hattori, K., Wallis, S., Enami,
M., Mizukami, T, 2007, Subduction of subarc mantle peridotites: Evidence from the Higashi-akaishi
garnet peridotites in the Sanbagawa
metamorphic belt,
Wang, J., Hattori, K.H., Kilian,
R., Stern,C.R., 2007, Metasomatism
of sub-arc mantle peridotites below southern
Hattori, K., 2007, Sulphur
and copper in magmatic arc: sources and linkages. Invited
presentation at the special session. American
Geophysical Union Meeting. V33F-01.,
pdf
Guillot, Replumaz,
A., Hattori, K.H., and Strzerzynski, P 2007, Initial geometry of western
Himalaya and ultra-high pressure metamorphic evolution. Journal
of Asian Earth Science vol. 30, p. 557-564. pdf file
Gorczyk, W., Guillot
S., Gerya, T.V., Hattori, K.H., 2007, Asthenospheric upwelling, oceanic
slab retreat and exhumation of UHP mantle rocks: insights from
Hattori, K. H., and Guillot, S., 2007, Geochemical character of serpentinites associated with high- to ultrahigh-pressure
metamorphic rocks in the Alps,
Guillot, S., Gerya, T.V., Gorczyk, W.,
Hattori, K., Schwartz, S., Saumur, B., Vidal, O., 2007. Exhumation of HP and UHP Rocks in Oceanic and Continental Subduction
Zones. American Geophysical Union Fall Meeting. V44A-03
Saumur, B-M, Hattori, K.H.
and Guillot, S., 2007, Geochemistry
of serpentinites from the northern subduction complex of
Deschamps, Fabien., Guillot, S., Godard, M.,
Hattori, K.H., Saumur, B.M., 2007, Subduction-related serpentinites:
New insights from Microprobe and Laser ICP-MS analyses on serpentine
minerals, Subduction Zone Geodynamics Meeting,
Montpellier, June
2007.
Guillot, S., Vidal,
O., Agard, P., Hattori, K., and Schwartz,S.,
2007, Exhumation
of HP to UHP rocks: constraints from petrological
studies and numerical modelling, Subduction Zone Geodynamics Meeting,
Montpellier, June 2007
Pettigrew, N.T. and Hattori, K.H.,
2006, The Quetico intrusions of the western
Wang, J., Hattori, K. and
Wang, J., Hattori,
K.H., Kilian, R., Stern,C.R., 2005,
Reduced fO2 recorded in the metasomatized peridotite xenoliths from the Sub-arc mantle in the
Southern most South
Saumur, B.-M., Hattori,
K.H., Guillot, S., 2006, Origin of hydrated peridotites associated with ultra high-pressure eclogites in
Hattori,
K., Takahashi, Y., Guillot, S. and Johanson, B. 2005, Occurrence
of arsenic (V) in fore-arc mantle serpentinites based on
X-ray absorption spectroscopy study,
Geochimica
et Cosmochimica Acta, vol.
69, p. 5585-5596. pdf file.
Guillot,
S., Schwartz, S., Hattori, K., Auzende, A. and Lardeaux, J. 2004.
The Monviso ophiolitic
Massif (
Wang J, Hattori H K,
Stern, C., 2004, Platinum-group
elements and oxidation of Paleozoic sub-continental lithospheric
mantle in southernmost South America: Xenolith study
in the Pali-Aike region,
Hattori, K., Takahashi, Y., Guillot, S. and Johanson,
B., 2004, Oxidized As (V) in fore-arc mantle serpentinites: Transfer of fluid-soluble elements from
slabs to arc magmas. Amer. Geophysical Union.
Fall Meeting, V13A-1439
Hattori,
K. and Guillot, S., 2003, Volcanic fronts as a consequence of serpentinite dehydration in the mantle wedge. Geology,
vol. 31, p. 525-528 click
for download.
Hoog, C.J., Hattori, K.H., 2003, Transfer of
sulphur from the mantle by oxidized mafic magma;
evidence from Mt. Pinatubo. Goldschmidt Conference in
Guillot,
S., Hattori, K., de Sigoyer, J., Nägler,
T., Auzende, A.L., 2001,
Evidence of hydration of the mantle wedge and its role in the
exhumation of eclogites. Earth and Planetary Science
Letters, vol. 193, p. 115-127. pdf file
Guillot,
S., Hattori, K.H. and de Sigoyer, J. 2000, Mantle wedge serpentinization
and exhumation of eclogites: Insights from eastern Ladakh, NW Himalaya.
Geology, vol
28, p. 199-202. pdf file
Hattori, K., Arai, S., Francis, D.M. & Clarke,
D.B., 1992, Variations of siderophile and chalcophle trace
elements among mantle-derived sulphides detected by in-situ
micro-PIXE analysis; EOS Transaction, American Geophysical Union, vol
73, p.344.
Primitive arc magmas and other subduction
-related publications
Hattori,
K., Hanyu, T., Stern, C.R., Tatsumi,
Y. and Nakai, S., 2005, Hafnium isotope evidence for the contribution of crustal
rocks at the source in the Andean Austral volcanic zone. European Union of Geoscience Meeting. EGU05-A-05955,
abstract
De Hoog, J.C.M., Hattori, K.H. and Hoblitt, R.P. 2004, Oxidized, sulfur-rich
mafic magma at Mount Pinatubo, Philippines, Contributions
to Mineralogy and Petrology, vol.
146,p. 750-761. click for download
Hattori, K.H.,Cabri, L.J., Johanson,
B., and Zientek,
M.L., 2004, Origin of placer laurite from
Hattori, K., DeHoog, C.J., Keith, J., 2004, Source of sulphur and
metals for giant porphyry copper deposits: contribution from oxidized mafic magmas. Invited, Annual Mtg.
Resource Geologists, Tokyo.
Hoog, C.J.and Hattori, K.H., 2003, Melt inclusion study of
trace metal behaviour during degassing of basaltic magma at Miyake-jima volcano (Izu-Bonin arc,
Hattori, K.H., Guillot, S., and Ishii, T., 2003,
Fore-arc mantle serpentinites as a reservoir of
fluid-soluble elements released from subducting
slabs. Goldschmidt Conference in
Hattori, K., de Hoog, J.C.M., Keith, J.D., Skewes, M.A., Stern, C.R., 2003, Oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinaubo,
Hattori, K.H., Guillot, S., and Ishii, T., 2003,
Fore-arc mantle serpentinites as a reservoir of
fluid-soluble elements released from subducting
slabs. Goldschmidt Conference in
Hattori, K.H. and Guillot, S.,
2003, Volcanic fronts as a consequence of serpentinite
dehydration in the mantle wedge., Joint
Assembly of European Geophysical Society, American Geophysical Union and
European Union of Geology, Geophysical Research Abstracts, v. 5,
EAE03-A-03536
De Hoog, JCM, Hattori, K.H., Hoblitt, R., 2003. Sulfur-rich, oxidized magma at
Hoog, C.J., Hattori, K.H., 2003, Transfer of
sulphur from the mantle by oxidized mafic magma;
evidence from Mt. Pinatubo. Goldschmidt Conference in
Hattori,
K.H., Arai, S., and Clarke, D.B., 2002, Selenium, tellurium, arsenic and
antimony contents in primary mantle sulfides. Canadian Mineralogist, vol. 40, no. 2,
637-650. click for pdf.
Maughan D.T., Keith,
J.D., Christiansen E.H., Pulsipher, T., Hattori K., and Evans, N.J., 2002, Contributions from mafic
alkaline magmas to the Bingham porphyry Cu-Au-Mo deposit, Utah, USA., Mineralium Deposita, vol. 37, p.14-37, pdf file
Hattori, K., De Hoog, JCM, Keith, J., 2002, Role of oxidized, S-rich magma for porphyry copper
mineralization, invited talk, Annual
Geological Society of
Hattori,
K.H. and Keith, J.D., 2001, Contribution of mafic
melt for porphyry deposits; evidence from Pinatubo and Bingham. Mineralium Deposits, vol. 36, no. 8, p. 799-806. Click for
download of pdf file.
Hattori, K. 1997, Occurrence
of sulphide and sulphate in
the 1991 Pinatubo eruption products and their origin.IN
Bernard, A., Knittel,
U., Weber, B., Weis, D., Albrecht, A., Hattori, K. , Klein, J. and Oles, D., 1997, Petrology and geochemistry of the
1991 eruption products of Mt. Pinatubo .IN
Keith, J.D., Whitney, J.A., Hattori, K., Ballantyne, G.H., Christianse,
E.H., Barr, D.L., Cannan, T.M. and Hook, C.J., 1997,
The role of magmatic sulphides and mafic alkaline magmas in the Bingham and Tintic mining districts,
Waite, K.A., Keith, J.D.,
Christiansen, E.H., Whitney, J.A., Hattori, K., Tingey,
D.G., Hook, C.J., 1997, Petrogenesis of the
volcanic and intrusive rocks associated with the Bingham porphyry Cu-Au-Mo
deposit, Utah. In: Geology and
Hattori,
K. and Sato, H., 1996, Magma Evolution Recorded in Plagioclase Zoning in
1991 Pinatubo Eruption Products. American Mineralogist, vol.
81, pp. 982-994. pdf file
Keith, J.D.,
Wait, K., Christianse, E.H., Tingey,
D.G., Nelson, S.T., Moore, D.K. and Hattori, K. 1997, What porphyry deposits may inherit from mafic
alkaline magmas, Bingham and Tintic districts, Utah: Volcnic activity and the environment, IAVCEI. Abst., p. 81.
Collins, C. and Hattori,
K., 1996, Role of magma mixing in
the 1200 ybp eruption of
Collins, C., Hattori, K.
and Stix, J., 1995, Incursion of hot
mafic magma into an evolved magma chamber beneath Galeras Volcano(
Keith, J.D., Whitney, J.A., Cannan, T.M., Hook, C.J., Hattori, K., 1995, The role of magmatic sulphides and mafic alkaline magmatism in the
formation of giant porphyry and vein systems; examples from the Bingham and Tintic Mining districts, Utah. Qmin
Ex. Symposium, Controls on the scale of hydrothermal activity associated with orogenic magmatism. .April,
Queen's Univ. 23pp.
Keith, J.D.,
Waite, K.A. and Hattori, K., 1994,
The origin and fate of magmatic sulfides in rocks associated with porphyry
copper and mesothermal vein deposits, Bingham and
East Tintic Mountains Mining Camps. 5th International
IAGOD Meeting,
Hattori, K., 1993,
Sulfides in the 1991 Pinatubo eruption products and the origin of highly
oxidized, sulfur-rich magma, EOS Trans. Amer. Geophysical Union,
vol. 74, no. 43, p.668.
Hattori, K. 1993,
High-sulfur magma, a product of fluid discharge from underlying mafic magma: Evidence from
Sato, H.,
Hattori, K. and Nakada, S., 1993, Contrasting
styles of magma interaction at Unzen and Pinatubo:
evidence from zonings of plagioclase, EOS,
Transaction American Geophysical
Hattori, K., Knittel, U. and Hoefs, J., 1992, Isotope study of S-rich, hydrated magmas from Mount Pinatubo,
Philippines, International Geological
Congress, vol.2, p.507
Knittel, U., Hattori, K., Hoefs, J., Oles,
D., 1992, Isotopic compositions of
anhydrite phenocryst-bearing pumices from the 1991
eruption of Mount Pinatubo, Philippines, EOS
Transaction American Geophysical Union,
vol. 73, p.342