A possibility of 18O-depleted oceans in the Precambrian inferred from triple oxygen isotope of shales and oceanic crust
- Award ID(s):
- 1833420
- NSF-PAR ID:
- 10349968
- Date Published:
- Journal Name:
- Chemical Geology
- Volume:
- 604
- Issue:
- C
- ISSN:
- 0009-2541
- Page Range / eLocation ID:
- 120944
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
More Like this
No document suggestions found
- Free Publicly Accessible Full Text
-
Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.1016/j.chemgeo.2022.120944
