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- Q902322 subject Q19845947.
- Q902322 subject Q19845948.
- Q902322 subject Q8516612.
- Q902322 subject Q8668311.
- Q902322 abstract "The Phoenix Plate (also known as the Aluk or Drake Plate) was an ancient tectonic plate that existed during the mid-Cretaceous through early Cenozoic time. The remainder of the plate is now located east of the Drake Passage/Shackleton Fracture Zone.The Phoenix Plate began subducting under the Antarctic Plate. The Phoenix Ridge, a mid-oceanic ridge between the Pacific and the Phoenix Plates which had a spreading rate of 18–20 cm per year until around 84 Ma. A major decrease in spreading rate, and the convergence rate with the Antarctic Plate occurred around 52.3 Ma. During the Late Cretaceous, the Phoenix Plate fragmented into the Charcot Plate, much in the same way in which the Rivera and the Cocos Plate were formed by the fragmentation of the Farallon Plate.The Antarctic-Phoenix Ridge (sometimes also called the Phoenix Ridge) consists of three extinct spreading ridge segments between the Antarctic Peninsula and the Scotia Sea. This ridge was initiated during the Late Cretaceous-Early Tertiary when the plate had divergent boundaries with the Bellingshausen and Pacific Plates. Bellingshausen was fused with the Antarctic Plate around 61 Ma and the Phoenix plate was gradually subducted by the Antarctic Plate as the Pacific-Antarctic Ridge propagated. The last collision between ridge crest segments and the subduction zone happened around 6.5 Ma and spreading had ceased entirely by 3.3 Ma when the small remnant of the Phoenix Plate was incorporated into the Antarctic Plate. The South Shetland Trench is the south-eastern boundary of the remnant and the Shackleton Fracture Zone is its north-eastern boundary.".
- Q902322 wikiPageExternalLink Eag2003c.pdf.
- Q902322 wikiPageWikiLink Q102416.
- Q902322 wikiPageWikiLink Q104698.
- Q902322 wikiPageWikiLink Q1200508.
- Q902322 wikiPageWikiLink Q1203170.
- Q902322 wikiPageWikiLink Q143650.
- Q902322 wikiPageWikiLink Q176318.
- Q902322 wikiPageWikiLink Q185605.
- Q902322 wikiPageWikiLink Q19845947.
- Q902322 wikiPageWikiLink Q19845948.
- Q902322 wikiPageWikiLink Q204703.
- Q902322 wikiPageWikiLink Q205411.
- Q902322 wikiPageWikiLink Q338199.
- Q902322 wikiPageWikiLink Q3391669.
- Q902322 wikiPageWikiLink Q386615.
- Q902322 wikiPageWikiLink Q44626.
- Q902322 wikiPageWikiLink Q501705.
- Q902322 wikiPageWikiLink Q5074185.
- Q902322 wikiPageWikiLink Q577.
- Q902322 wikiPageWikiLink Q7186973.
- Q902322 wikiPageWikiLink Q7460183.
- Q902322 wikiPageWikiLink Q7950.
- Q902322 wikiPageWikiLink Q8516612.
- Q902322 wikiPageWikiLink Q8668311.
- Q902322 comment "The Phoenix Plate (also known as the Aluk or Drake Plate) was an ancient tectonic plate that existed during the mid-Cretaceous through early Cenozoic time. The remainder of the plate is now located east of the Drake Passage/Shackleton Fracture Zone.The Phoenix Plate began subducting under the Antarctic Plate. The Phoenix Ridge, a mid-oceanic ridge between the Pacific and the Phoenix Plates which had a spreading rate of 18–20 cm per year until around 84 Ma.".
- Q902322 label "Phoenix Plate".