- (alt) ·
Bluebook (alt) NLM (alt) ·
MathSciNet (alt ) ISO 4 J. Volcanol.
Geotherm. Res.
Indexing CODEN (alt · alt2) ·
JSTOR (alt) · LCCN (alt) MIAR · NLM...
- zone re-configuration as a
precursor to
flank instability. J. Volcanol.
Geotherm Res. 94, 135–167., Ward, S. N. & Day, S. J; 2001. ****bre
Vieja Volcano;...
- high
pressure TTGs have
experienced geotherms lower than 10 °C/km,
which are
close to
modern hot
subduction geotherms experienced by
young slabs (but around...
-
control on the
growth of
large oceanic-island volcanoes". J. Volcanol.
Geotherm Res. 60, 225–241. Carracedo, J. C; 1999. "Growth, Structure, Instability...
-
Geothermal gradient is the rate of
change in
temperature with
respect to
increasing depth in Earth's interior. As a
general rule, the
crust temperature...
- re-configuration as a
precursor to
flank instability" (PDF). J. Volcanol.
Geotherm. Res. 94 (1–4): 135–167. Bibcode:1999JVGR...94..135D. CiteSeerX 10.1.1...
- such as
serpentine can be
stable at
different pressures within the slab
geotherms, and may
transport significant amount of
water into the Earth's interior...
- evolution, with a
special emphasis to the
major pyroclastic events. J Volc
Geotherm Res, 100: 139–163
Charbonnier S J,
Gertisser R, 2008.
Field observations...
- and S-wave
velocities (Vp and Vs) of
pyrolite along the 1600 K
adiabatic geotherm are
shown in Fig. 2, and its
density profile is
shown in Fig. 3. At the...
- Jarvis, Gary T.; Campbell, Ian H. (December 1983). "Archean
komatiites and
geotherms:
Solution to an
apparent contradiction".
Geophysical Research Letters...
