In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 18, No. 12 ( 2017-12), p. 4503-4521
Abstract:
MCS data are integrated with grab samples and cores to constrain the history of uplift and subsidence of the eastern Mendocino transform fault from 8 to 0 Ma Uplift of a transform ridge formed from EW‐trending slices of oceanic crust began prior to 6 Ma, and the crest of the ridge was above sea level from ∼3.7 to 2.5 Ma Magmatic intrusion may have contributed to uplift and emergence, which likely led to enhanced upwelling, low SST, and high sedimentation rates south of the island
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2017GC007128
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2027201-7
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