Franciscan Complex limestone deposited at 17o south paleolatitude.

W. Alvarez, D. V. Kent, I. P. Silva, R. A. Schweickert, R. A. Larson

Research output: Contribution to journalArticlepeer-review

62 Scopus citations

Abstract

At Laytonville, California, 3 blocks of pelagic limestone, each a few tens of metres long, are incorporated in the Franciscan melange. Bedding is well defined, but top indicators are lacking. Study of foraminfera showed that the blocks are of Albian and Cenomanian age and were deposited during the Cretaceous Long Normal Polarity Interval. Details of the foraminiferal zonation show that both blocks are right side up. The observed inclinations imply deposition on the Farallon plate at 17o +/- 7o S paleolatitude at c.96 m.y. BP. Consideration of reasonable paleolongitudes and possible times of incorporation of the blocks in the melange indicates a Farallon-North America convergence rate significantly higher than any observed today.- from Authors

Original languageEnglish (US)
Pages (from-to)476-484
Number of pages9
JournalGeological Society of America, Bulletin
Volume91
Issue number8 pt. 1
StatePublished - 1980
Externally publishedYes

All Science Journal Classification (ASJC) codes

  • Geology

Fingerprint

Dive into the research topics of 'Franciscan Complex limestone deposited at 17o south paleolatitude.'. Together they form a unique fingerprint.

Cite this