Last Updated：2022/12/24
Next Reports Footwall Refrigeration Along a Detachment Fault: Implications for the Thermal Evolution of Core Complexes Jean Morrison, * J. Lawford Anderson Oxygen isotope compositions of epidote and quartz from chloritic breccias that underlie the detachment fault in the metamorphic core complex of the Whipple Mountains yielded quartz-epidote fractionations that range from 4.1 to 6.4 per mil and increase systematically toward the fault.
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Next
Reports
Footwall
Refrigeration
Along
a
Detachment
Fault:
Implications
for
the
Thermal
Evolution
of
Core
Complexes
Jean
Morrison,
*
J.
Lawford
Anderson
Oxygen
isotope
compositions
of
epidote
and
quartz
from
chloritic
breccias
that
underlie
the
detachment
fault
in
the
metamorphic
core
complex
of
the
Whipple
Mountains
yielded
quartz-epidote
fractionations
that
range
from
4.1
to
6.4
per
mil
and
increase
systematically
toward
the
fault.
