Glacial cycles drive variations in the production of oceanic crust

التفاصيل البيبلوغرافية
العنوان: Glacial cycles drive variations in the production of oceanic crust
المؤلفون: Crowley, John W., Katz, Richard F., Huybers, Peter J., Langmuir, Charles H., Park, Sung-Hyun
المصدر: Science, Vol. 347, no. 6227, pp. 1237-1240, 2015
سنة النشر: 2014
المجموعة: Physics (Other)
مصطلحات موضوعية: Physics - Geophysics
الوصف: Glacial cycles redistribute water between oceans and continents causing pressure changes in the upper mantle, with consequences for melting of Earth's interior. Using Plio-Pleistocene sea-level variations as a forcing function, theoretical models of mid-ocean ridge dynamics that include melt transport predict temporal variations in crustal thickness of hundreds of meters. New bathymetry from the Australian-Antarctic ridge shows significant spectral energy near the Milankovitch periods of 23, 41, and 100 ky, consistent with model predictions. These results suggest that abyssal hills, one of the most common bathymetric features on Earth, record the magmatic response to changes in sea level. The models and data support a link between glacial cycles at the surface and mantle melting at depth, recorded in the bathymetric fabric of the sea floor.
Comment: 30 pages, 6 figures (including supplementary information). Resubmitted to Science on 12 December 2014
نوع الوثيقة: Working Paper
DOI: 10.1126/science.1261508
الوصول الحر: http://arxiv.org/abs/1408.4976Test
رقم الانضمام: edsarx.1408.4976
قاعدة البيانات: arXiv