The orthogonal supersegment of the ultraslow-spreading Southwest Indian Ridge at 16°–25°E is characterized by significant along-axis variations of mantle potential temperature.A detailed analysis of multibe...The orthogonal supersegment of the ultraslow-spreading Southwest Indian Ridge at 16°–25°E is characterized by significant along-axis variations of mantle potential temperature.A detailed analysis of multibeam bathymetry,gravity,and magnetic data were performed to investigate its variations in magma supply and crustal accretion process.The results revealed distinct across-axis variations of magma supply.Specifically,the regionally averaged crustal thickness reduced systematically from around 7 Ma to the present,indicating a regionally decreasing magma supply.The crustal structure is asymmetric in regional scale between the conjugate ridge flanks,with the faster-spreading southern flank showing thinner crust and greater degree of tectonic extension.Geodynamic models of mantle melting suggested that the observed variations in axial crustal thickness and major element geochemistry can be adequately explained by an eastward decrease in mantle potential temperature of about40℃ beneath the ridge axis.In this work,a synthesized model was proposed to explain the axial variations of magma supply and ridge segmentation stabilities.The existence of large ridge-axis offsets may play important roles in controlling melt supply.Several large ridge-axis offsets in the eastern section(21°–25°E)caused sustained along-axis focusing of magma supply at the centers of eastern ridge segments,enabling quasi-stable segmentation.In contrast,the western section(16°–21°E),which lacks large ridge-axis offsets,is associated with unstable segmentation patterns.展开更多
基金The Program of Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)under contract No.GML2019ZD0205the National Natural Science Foundation of China under contract Nos 41890813,41976066,41976064,91858207,91958211 and 91628301+3 种基金the Program of Chinese Academy of Sciences under contract Nos Y4SL021001,QYZDY-SSW-DQC005 and133244KYSB20180029the National Key Research and Development Program of China under contract Nos 2018YFC0309800 and2018YFC0310105the Guangdong Basic and Applied Basic Research Foundation under contract No.2021A1515012227the Program of China Ocean Mineral Resources Research and Development Association under contract No.DY135-S2-1-04。
文摘The orthogonal supersegment of the ultraslow-spreading Southwest Indian Ridge at 16°–25°E is characterized by significant along-axis variations of mantle potential temperature.A detailed analysis of multibeam bathymetry,gravity,and magnetic data were performed to investigate its variations in magma supply and crustal accretion process.The results revealed distinct across-axis variations of magma supply.Specifically,the regionally averaged crustal thickness reduced systematically from around 7 Ma to the present,indicating a regionally decreasing magma supply.The crustal structure is asymmetric in regional scale between the conjugate ridge flanks,with the faster-spreading southern flank showing thinner crust and greater degree of tectonic extension.Geodynamic models of mantle melting suggested that the observed variations in axial crustal thickness and major element geochemistry can be adequately explained by an eastward decrease in mantle potential temperature of about40℃ beneath the ridge axis.In this work,a synthesized model was proposed to explain the axial variations of magma supply and ridge segmentation stabilities.The existence of large ridge-axis offsets may play important roles in controlling melt supply.Several large ridge-axis offsets in the eastern section(21°–25°E)caused sustained along-axis focusing of magma supply at the centers of eastern ridge segments,enabling quasi-stable segmentation.In contrast,the western section(16°–21°E),which lacks large ridge-axis offsets,is associated with unstable segmentation patterns.
