Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Oceanic plateaus: Problematic plumes, potential paradigms

Kerr, Andrew Craig and Mahoney, John J. 2007. Oceanic plateaus: Problematic plumes, potential paradigms. Chemical Geology 241 (3-4) , pp. 332-353. 10.1016/j.chemgeo.2007.01.019

Full text not available from this repository.

Abstract

Oceanic plateaus are vast areas (N2—105 km2) of thicker than average oceanic crust (up to 38 km) that typically are elevated 2-3 km above the surrounding seafloor. Because of their thick, relatively high-standing crust, portions of oceanic plateaus can accrete to convergent continental margins and thus have contributed to continental growth over time. Through studies of accreted oceanic plateau sections and from drilling of in-situ plateaus, knowledge of plateau structure, composition and age has increased considerably over the last 20 years. However, models for the origin of oceanic plateaus are still not without significant problems.Mantle plume models can explain many of the observed chemical and physical features, but other characteristics are not readily explicable by conventional thermal plume models. This is particularly true of the largest plateau, the Cretaceous Ontong Java Plateau in the western Pacific. If formed by a plume head, much of the surface of this plateau should have become subaerial, but instead largely appears to have erupted at water depths 1000 m; furthermore, post-eruption subsidence was much less than predicted by thermal plume models. Other models, such as meteorite impact-induced melting and spreading-induced upwelling of eclogite, are also fraught with problems. A solution to the anomalous uplift and subsidence of the Ontong Java Plateau may lie in its derivation from a thermo-chemical mantle plume. Modelling suggests such plumes can consist of large amounts of compositionally densematerial, thereby reducing net plume buoyancy. Future work should explore in detail the capabilities of thermochemical plumes, the role of oceanic plateaus in continental growth, and links between the formation of plateaus and major environmental crises such as oceanic anoxic events.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Subjects: Q Science > QE Geology
Uncontrolled Keywords: Ontong Java Plateau; Kerguelen Plateau; Caribbean Plateau; Thermochemical plume; Oceanic plateau
Publisher: Elsevier
Last Modified: 04 Jun 2017 01:53
URI: http://orca.cf.ac.uk/id/eprint/5296

Citation Data

Cited 48 times in Google Scholar. View in Google Scholar

Cited 76 times in Scopus. View in Scopus. Powered By Scopus® Data

Actions (repository staff only)

Edit Item Edit Item