Oxfordian magnetic polarity pattern-reply to comment by R.E. Sheridan and K.A. Suydam

Details Oxfordian magnetic polarity pattern-reply to comment by R.E. Sheridan and K.A. Suydam Oxfordian magnetic polarity pattern-reply to comment by R.E. Sheridan and K.A. Suydam

Sep 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987e%26psl..85..323s&link_type=abstract

Earth and Planetary Science Letters, Volume 85, Issue 1-3, p. 323-325.

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Scientific paper

Sheridan and Suydam [1] raise several important points, which are primarily related to the origin of reported magnetic anomalies within the Jurassic magnetic quiet zone of the ocean crust, and therefore are not directly relevant to our magnetostratigraphic study of Oxfordian sediments [2]. We will discuss only two points: (1) the consistency of our Oxfordian results with other evidence of mixed polarity, and (2) the factors complicating the resolution of rapid magnetic reversals in the anomaly record of deep Jurassic crust.

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