Temporal and spatial cyclicity of accretion at slow-spreading ridges—evidence from the Reykjanes Ridge.
Temporal and spatial cyclicity of accretion at slow-spreading ridges—evidence from the Reykjanes Ridge.
复制标题
缓慢扩张的山脊吸积的时间和空间周期性——来自雷克雅内斯山脊的证据。
DOI:
10.1111/j.1365-246x.2005.02738.x
复制
发表时间:
2005
影响因子:
2.8
通讯作者:
M. Sinha
中科院分区:
文献类型:
--
作者:
C. Peirce;A. Gardiner;M. Sinha
SUMMARY A unifying model of oceanic crustal development at slow spreading rates is presented in which accretion follows a cyclic pattern of magmatic construction and tectonic destruction, controlled by along-axis variation in melt supply and coupled to along-axis variation in spreading rate and across-axis asymmetry in spreading. This study focuses on the Reykjanes Ridge, Mid-Atlantic Ridge south of Iceland, which is divided along its entire length into numerous axial volcanic ridges (AVR). Five adjacent AVRs have been analysed, located between 57 ◦ 30 � N and 58 ◦ 30 � N and south of any strong Iceland hotspot influence. The seabed morphology of each AVR is investigated using sidescan sonar data to determine relative age and eruptive history. Along-axis gravity profiles for each AVR are modelled relative to a seismically derived crustal reference model, to reveal the underlying crustal thickness and density structure. Correlating these models with seabed features, crustal structure, ridge segment morphology and relative ages, a model of cyclic ridge segmentation is developed in which accretion results in adjacent AVRs with a range of crustal features which, when viewed collectively, reveal that second-order segments on the Reykjanes Ridge have an along-axis length of ∼70 km and comprise several adjacent AVRs which, in turn, reflect the pattern of third-order segmentation. Tectono-magmatic accretion is shown to operate on the scale of individual AVRs, as well as on the scale of the second-order segment as a whole.
DOI:
--
发表时间:
2002
期刊:
Earth Planet.Sci.Lett. 199
影响因子:
--
作者:
Sauter;D.;L.Parson;V.Mendel;C.Rommevaux-Jestin;O.Gomez;A.Briais;C.Mevel;K.Tamaki;FUJI scientific team
通讯作者:
FUJI scientific team