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Issues

ISSN 0091-7613
EISSN 1943-2682
In this Issue
Geology August 01, 1980, Vol.8, 354. doi:https://doi.org/10.1130/0091-7613(1980)8<354:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 355. doi:https://doi.org/10.1130/0091-7613(1980)8<355a:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 355-356. doi:https://doi.org/10.1130/0091-7613(1980)8<355b:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 356-357. doi:https://doi.org/10.1130/0091-7613(1980)8<356:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 357-359. doi:https://doi.org/10.1130/0091-7613(1980)8<357:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 359. doi:https://doi.org/10.1130/0091-7613(1980)8<359:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 360. doi:https://doi.org/10.1130/0091-7613(1980)8<360a:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 360-361. doi:https://doi.org/10.1130/0091-7613(1980)8<360b:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 361-362. doi:https://doi.org/10.1130/0091-7613(1980)8<361:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 362-364. doi:https://doi.org/10.1130/0091-7613(1980)8<362:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 364-365. doi:https://doi.org/10.1130/0091-7613(1980)8<364:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 365-367. doi:https://doi.org/10.1130/0091-7613(1980)8<365:CAROCP>2.0.CO;2
Geology August 01, 1980, Vol.8, 368-370. doi:https://doi.org/10.1130/0091-7613(1980)8<368:RGSATU>2.0.CO;2
Geology August 01, 1980, Vol.8, 371-374. doi:https://doi.org/10.1130/0091-7613(1980)8<371:AAOSPP>2.0.CO;2
Geology August 01, 1980, Vol.8, 375-379. doi:https://doi.org/10.1130/0091-7613(1980)8<375:TSOEOP>2.0.CO;2
Geology August 01, 1980, Vol.8, 380-384. doi:https://doi.org/10.1130/0091-7613(1980)8<380:IAAPFT>2.0.CO;2
Geology August 01, 1980, Vol.8, 385-389. doi:https://doi.org/10.1130/0091-7613(1980)8<385:UJTLCS>2.0.CO;2
Geology August 01, 1980, Vol.8, 390-395. doi:https://doi.org/10.1130/0091-7613(1980)8<390:MIOSVH>2.0.CO;2
Geology August 01, 1980, Vol.8, 396-400. doi:https://doi.org/10.1130/0091-7613(1980)8<396:IOMRDF>2.0.CO;2
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