Главная
Study mode:
on
1
Introduction
2
Motivation
3
How cherts form
4
Opal A
5
Archean
6
Secondary Ion Probe
7
Temperature dependent fractionation
8
Altered basalts
9
Measurement strategy
10
Data collection
11
Comparison diagram
12
Another example
13
Best preserved samples
14
Data compilation
15
Primary signatures
16
Secondary processes
17
Primary marine silica
18
Global compilation of charts
19
Changing seawater composition
20
Generalized interpretation
21
Conclusions
22
What would it suggest
Description:
Explore the temporal triple oxygen isotope trend recorded in Precambrian cherts through this 34-minute conference talk presented at the Mineralogical Society of America's Short Course on Triple Oxygen Isotope Geochemistry. Delve into the formation of cherts, Archean opal A, and the use of secondary ion probes for analysis. Examine temperature-dependent fractionation, altered basalts, and measurement strategies. Analyze data collection methods, comparison diagrams, and examples of best-preserved samples. Investigate primary signatures, secondary processes, and the global compilation of charts. Discuss changing seawater composition and its generalized interpretation. Conclude with insights into the implications of this research for understanding Earth's early environment and geological processes.

Temporal Triple Oxygen Isotope Trend Recorded by Precambrian Cherts

Mineralogical Society of America
Add to list