Fastest known spreading on the Miocene Cocos‐Pacific plate boundary
DS Wilson - Geophysical Research Letters, 1996 - Wiley Online Library
New magnetic anomaly identifications for the central part of the Cocos plate and the
corresponding part of the Pacific plate indicate a pulse of extremely rapid seafloor spreading
in the middle Miocene, about 11–18 Ma, possibly beginning as early as 25 Ma. The spacing
of anomalies 5A–5D indicates a full spreading rate for the southern Cocos‐Pacific boundary
of 180–210 mm/yr, depending on the choice of time scale. Relative to the maximum 0–3 Ma
spreading rate of 152 mm/yr, this result significantly expands the upper limit of well …
corresponding part of the Pacific plate indicate a pulse of extremely rapid seafloor spreading
in the middle Miocene, about 11–18 Ma, possibly beginning as early as 25 Ma. The spacing
of anomalies 5A–5D indicates a full spreading rate for the southern Cocos‐Pacific boundary
of 180–210 mm/yr, depending on the choice of time scale. Relative to the maximum 0–3 Ma
spreading rate of 152 mm/yr, this result significantly expands the upper limit of well …
Fastest known spreading on the Miocene Cocos-Pacific plate boundary
DS Wilson - Oceanographic Literature Review, 1997 - infona.pl
New magnetic anomaly identifications for the central part of the Cocos plate and the
corresponding part of the Pacific plate indicate a pulse of extremely rapid sea-floor
spreading in the middle Miocene, about 11-18 Ma, possibly beginning as early as 25 Ma.
The spacing of anomalies 5A-5D indicates a full spreading rate for the southern Cocos-
Pacific boundary of 180-210 mm/yr, depending on the choice of time scale.
corresponding part of the Pacific plate indicate a pulse of extremely rapid sea-floor
spreading in the middle Miocene, about 11-18 Ma, possibly beginning as early as 25 Ma.
The spacing of anomalies 5A-5D indicates a full spreading rate for the southern Cocos-
Pacific boundary of 180-210 mm/yr, depending on the choice of time scale.
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