Vestnik Kamchatskoy regional'noy assotsiatsii «Uchebno-nauchnyy tsentr». Seriya: Nauki o Zemle
Institute of Volcanology and Seismology FEB RAS
Peculiarities of ultraslow spreading during the formation and development of spreading systems
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Keywords

ultraslow spreading
sea floor relief
structure formation
divergent plate boundaries

Section

Results of the Scientific Researches

Abstract

Main geodynamic environments of ultra-slow spreading on divergent plate boundaries are considered in this paper. Ultra-slow spreading can occur now or could occur in the past in the following geodynamic environments on divergent plate boundaries: 1. on spreading ridges with ultra-slow spreading, both modern and ceased; 2. during transition from continental rifting to early stages of oceanic spreading (all spreading ridges during incipient stages of their formation); 3. during incipient stages of formation of spreading ridges on oceanic crust as a result of ridge jumps and reorganization of plate boundaries; 4. during propagation of spreading ridge into the continental crust caused by a hotspot and strike-slip faults preceding the propagation.

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