Tectonic evolution and midplate volcanism in the South Pacific
Jordahl, Kelsey A.
MetadataShow full item record
KeywordStructural geology; Plate tectonics; Volcanism; Maurice Ewing (Ship) Cruise EW9109; Maurice Ewing (Ship) Cruise EW9602; Roger Revelle (Ship) Cruise KIWI03
Changes in morphology of the Marquesas Fracture Zone are correlated with small changes in Pacific-Farallon relative motion. The simple flexural signal of a locked fracture zone may be obscured by tectonic effects, and there is no evidence for the release of shear stress on the fracture zone by vertical slip after leaving the active transform. One such small change in plate motion is documented in the South ern Austral Island region of the South Pacific. A twelve degree clock wise change in Pacific-Farallon relative motion occurred around fifty million years ago. This Eocene change in spreading direction and rate is locally constrained with observations of magnetic anomalies and spreading fabric orientation. At the southeastern end of the Cook-Austral Island chain, multiple episodes of volcanism have left a diverse population of seamounts. Volume estimates from geophysical data and modeling show that one-half to two-thirds of the volcanic material is over thirty million years old, while the remainder is less than five million years old. Seismic and bathymetric data imply the presence of abyssal basalt flows in the flexural moat of the Austral Islands, probably associated with Austral Islands volcanism, which may contribute a significant amount of material to the archipelagic apron.
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 1999
Suggested CitationThesis: Jordahl, Kelsey A., "Tectonic evolution and midplate volcanism in the South Pacific", 1999-02, DOI:10.1575/1912/4688, https://hdl.handle.net/1912/4688
Showing items related by title, author, creator and subject.
Cann, Johnson R.; Smith, Deborah K. (American Geophysical Union, 2005-09-09)We reconstruct the volcanic and tectonic evolution over the last 250,000 years of the median valley floor in the spreading segment of the Mid-Atlantic Ridge centered at 25°N. In the center of the segment, multibeam bathymetry ...
Interplay between faults and lava flows in construction of the upper oceanic crust : the East Pacific Rise crest 9°25′–9°58′N Escartin, Javier E.; Soule, Samuel A.; Fornari, Daniel J.; Tivey, Maurice A.; Schouten, Hans A.; Perfit, Michael R. (American Geophysical Union, 2007-06-07)The distribution of faults and fault characteristics along the East Pacific Rise (EPR) crest between 9°25′N and 9°58′N were studied using high-resolution side-scan sonar data and near-bottom bathymetric profiles. The ...
Tominaga, Masako; Tivey, Maurice A.; Sager, William W. (John Wiley & Sons, 2015-10-24)The nature of the Jurassic Quiet Zone (JQZ), a region of low-amplitude oceanic magnetic anomalies, has been a long-standing debate with implications for the history and behavior of the Earth's geomagnetic field and plate ...