Abstract

Well-preserved underplating structure of the jadeitized Franciscan complex, Pacheco Pass, California: Correction

Geology, v. 24, p. 75–78 (January 1996)

Longitude lines were incorrectly identified on the map in Figure 2 of our article. This figure is reprinted below with the corrected longitude coordinates. We are indebted to M. C. Erskine for bringing this to our attention.  
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CORRECTION

Alternate interpretation of the Messinian salinity crisis: Controversy resolved?: Correction

Geology, v. 24, p. 363–366 (April 1996)

On p. 364, the first sentence of the second paragraph under the heading THE SALINITY CRISIS: FROM ABYSSAL PLAINS TO MARGINS should be:

Peripheral basins have evaporites that are estimated to be in the earliest Pliocene (Fig. 2A) 2000 to 3000 m above the deep-basin evaporites (modern difference in elevation, 4000 to 5000 m); surprisingly, these two kinds of evaporites have been considered as similar and coeval (Nesterhoff, 1973; Ryan, 1973).

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