A fossilized Opal A to Opal C/T transformation on the northeast Atlantic margin: support for a significantly elevated Palaeogeothermal gradient during the Neogene?-Reference-Cited by-同舟云学术

A fossilized Opal A to Opal C/T transformation on the northeast Atlantic margin: support for a significantly elevated Palaeogeothermal gradient during the Neogene?

Published:2002-12 Issue:4 Volume:14 Page:467-486
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:

Author:

Davies R. J.,Cartwright J.

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1046/j.1365-2117.2002.00184.x/fullpdf

Reference52 articles.

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2. Pure siliceous ooze, a diagenetic environment for early chert formation;Bohrmann;Geology,1994

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