Skip to main navigation
Skip to search
Skip to main content
Okayama University Home
Home
Researcher Profiles
Research Units
Research output
Activities
Press / Media
Prizes
Search by expertise, name or affiliation
Nitrogen isotope tracers of high-temperature fluid-rock interactions: Case study of the Catalina Schist, California
Gray E. Bebout
Research output
:
Contribution to journal
›
Article
›
peer-review
58
Citations (Scopus)
Overview
Fingerprint
Fingerprint
Dive into the research topics of 'Nitrogen isotope tracers of high-temperature fluid-rock interactions: Case study of the Catalina Schist, California'. Together they form a unique fingerprint.
Sort by
Weight
Alphabetically
Physics & Astronomy
crusts
6%
Earth mantle
6%
fluids
25%
fractionation
6%
grade
20%
high temperature fluids
95%
interactions
21%
isotopes
32%
mass balance
13%
mica
24%
muscovite
15%
nitrogen isotopes
95%
oxygen isotopes
7%
rocks
52%
schist
100%
sediments
6%
silicates
10%
tracers
52%
veins
6%
Earth & Environmental Sciences
albite
7%
crust
5%
fluid
31%
fractionation
5%
isotope
30%
lawsonite
9%
leucosome
9%
mass balance
12%
metamorphism
5%
mica
27%
migmatization
9%
muscovite
14%
nitrogen isotope
62%
oxygen isotope
6%
pegmatite
15%
rock
26%
schist
54%
silicate melt
16%
stable isotope
5%
subduction zone
13%
tracer
42%
ultramafic rock
7%
Chemical Compounds
Flow
17%
Fractionation
23%
Isotope
46%
Mass Balance
64%
Reaction Yield
22%
Stable Isotope
29%
White
22%