Environmental Engineering Reference
In-Depth Information
-
Etendeka Large Igneous Province. Earth and
environmental impact of the Paraná
49.
Marty, B. and Tolstikhin, I.N. (1998). CO 2
Planetary Science Letters , 392,39
-
fluxes from mid-ocean ridges, arcs and plumes.
248.
Mason, B.G., Pyle, D.M. and Oppenheimer, C. (2004a). The size and frequency of the
largest eruptions on Earth. Bulletin of Volcanology , 66, 735
Chemical Geology , 145, 233
-
748.
Mason, B.G., Pyle, D.M., Dade, W.B. and Jupp, T. (2004b). Seasonality of volcanic
eruptions. Journal of Geophysical Research , 109, B04206.
Mather, T.A., Pyle, D.M. and Oppenheimer, C. (2003). Tropospheric volcanic aerosol.
AGU Geophysical Monograph , 139, 189
-
212.
McCormick M.P., Thomason, L.W. and Trepte, C.R. (1995). Atmospheric effects of the
Mt. Pinatubo eruption. Nature , 373, 399
-
404.
McGuire, W.J., Howarth, R.J., Firth, C.R. et al . (1997). Correlation between rate of sea-
level change and frequency of explosive volcanism in the Mediterranean. Nature ,
389, 473
-
476.
Miller, G.H., Geirsdóttir, Á., Zhong, Y.F. et al . (2012). Abrupt onset of the Little Ice Age
triggered by volcanism and sustained by sea-ice/ocean feedbacks. Geophysical
Research Letters , 39, L02708.
Moretti, R., Papale, P. and Ottonello, G. (2003). A model for the saturation of
C
-
fluids in silicate melts. Geological Society of London Special Publica-
tion , 213,81
-
O
-
H
-
S
101.
Nakada, M. and Yokose, H. (1992). Ice-age as a trigger of active quaternary volcanism and
tectonism. Tectonophysics , 212, 321
-
-
329.
Nowell, D.A.G., Jones, M.C. and Pyle, D.M. (2006). Episodic Quaternary volcanism in
France and Germany. Journal of Quaternary Science , 21, 645
-
675.
Oppenheimer, C. (2002). Limited global change due to the largest known Quaternary
eruption, Toba
1609.
Oppenheimer, C. (2003). Climatic, environmental and human consequences of the largest
known historic eruption: Tambora volcano (Indonesia) 1815. Progress in Physical
Geography , 27,230
~
74 kyr BP? Quaternary Science Reviews , 21, 1593
-
259.
Pagli, C. and Sigmundsson, F. (2008). Will present day glacier retreat increase volcanic
activity? Stress induced by recent glacier retreat and its effect on magmatism at the
Vatnajokull ice cap, Iceland. Geophysical Research Letters , 35, L09304.
Parks, M.M., Caliro, S., Chiodini, G. et al . (2013). Distinguishing contributions to diffuse
CO 2 emissions in volcanic areas from magmatic degassing and thermal decarbonation
using soil gas
-
13 C systematics: application to Santorini volcano, Greece.
Earth and Planetary Science Letters , 377
222 Rn
- δ
190.
Paterson, S.R., Okaya, D., Memeti, V., Economos, R. and Miller, R.B. (2011). Magma
addition and
-
378, 180
-
flux calculations of incrementally constructed magma chambers in
continental margin arcs: combined
field, geochronologic, and thermal modeling
studies. Geosphere , 7, 1439
-
1468.
Petraglia, M., Ditch
eld, P., Jones, S., Korisettar, R. and Pal, J.N. (2012). The Toba
volcanic super-eruption, environmental change and hominin occupation history in
India over the last 140,000 years. Quaternary International , 258, 119
134.
Pyle, D.M. (1995). Mass and energy budgets of explosive volcanic eruptions. Geophysical
Research Letters , 22, 563
-
566.
Pyle, D.M., Beattie, P.D. and Bluth, G.J.S. (1996). Sulphur emissions to the stratosphere
from explosive volcanic eruptions. Bulletin of Volcanology , 57, 663
-
-
671.
Pyle, D.M. and Mather, T.A. (2003). The importance of volcanic emissions in the global
atmospheric mercury cycle. Atmospheric Environment , 37, 5115 - 5124.
Search WWH ::




Custom Search