- The
Taltson magmatic zone (TMZ) is a north-trending belt of
Archean to
Paleoproterozoic granitic ba****t gneiss,
amphibolite supracrustal gneissic rock...
-
Magmatic water, also
known as
juvenile water, is an
aqueous phase in
equilibrium with
minerals that have been
dissolved by
magma deep
within the Earth's...
-
spans more than 7 million years. It has
taken place during five
cycles of
magmatic activity, each
producing less
volcanic material than the
previous one....
-
Magmatic underplating occurs when
basaltic magmas are
trapped during their rise to the
surface at the Mohorovičić
discontinuity or
within the crust. Entrapment...
- A
magmatic lull is a
period of
declined magmatic activity in
volcanically active regions. They may
occur as a
result of
underthrusting of
hinterland lithosphere...
-
Magmatic foliation is a term in geology, for
foliation in
granitoids that form by
magmatic flow, "submagmatic flow," by high-temperature solid-state deformation...
-
exclusively magmatic eruptions and
phreatic eruptions.
Unlike phreatic eruptions, the
products of
phreatomagmatic eruptions contain juvenile (
magmatic) clasts...
-
terrestrial planet,
which solidifies as
igneous rocks. It does so
through magmatic activity or
igneous activity, the production,
intrusion and
extrusion of...
- The
Central Atlantic magmatic province (CAMP) is the Earth's
largest continental large igneous province,
covering an area of
roughly 11
million km2. It...
- one
eruptive series.
There are
three main
types of
volcanic eruption:
Magmatic eruptions are the most well-observed type of eruption. They
involve the...
