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Analysis of a north-south magnetic profile over the Central Indian Ocean

机译:中印度洋上南北磁剖面的分析

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Marine magnetic anomalies provide valuable information on the nature and evolution of the oceanic crust, Magnetic profiles aligned along the direction of spreading enable us to calculate the spreading rates of oceanic crusts on which they pass. This can he done with computed profiles assuming the model and magnetic reversal time scale of the earth. In the present study the north-south magnetic profile of 1280 nautical miles extending from 15 degrees 30'S, 77 degrees E to 6 degrees N, 79 degrees E in the Central Indian Ocean is analysed. The profile runs between the 76 degrees 30'E and 79 degrees E Fracture Zones passing over part of the Australian plate, the Central Indian Ocean deformation zone and part of the Indian plate along the Comorin Ridge. The analysis shows that the profile has a continuous sequence of prominent age anomalies from 22 to 34 N. Australian plate and deformation zone segments have well preserved continuous age anomalies from 22 to 33 and thus their spreading rates are calculated. The results show that the profile is characterized by sets of anomalies with varied spreading rates, anomalies 23-30 having higher values compared to the rest. The spreading rate of anomalies 22-27 is 7.8 cm/yr whereas for anomalies 27-30 it is 10.3 cm/yr. Anomalies 30-33 have a moderate spreading rate of 4.6 cm/yr. Another interesting feature is that the profile has the characteristic edge-effect anomaly on the segment over the Indian plate indicating the oceanic-continental crust boundary. [References: 31]
机译:海洋磁异常为洋壳的性质和演化提供了有价值的信息。沿传播方向排列的磁剖面使我们能够计算出它们经过的洋壳的传播速率。这可以通过假设地球的模型和磁逆时标的计算轮廓来完成。在本研究中,分析了中印度洋从15度30',77度E到6度N,79度E延伸的1280海里的南北磁剖面。剖面在76度30'E和79度E断裂带之间延伸,穿过澳大利亚板块的一部分,中印度洋变形带和沿科摩林岭的印度板块的一部分。分析表明,该剖面具有从22到34 N的突出的年龄异常的连续序列。澳大利亚板块和变形带段保存了从22到33的良好的连续年龄异常,因此计算了它们的扩散率。结果表明,该剖面的特征是具有不同扩展率的异常集,与其他异常相比,异常23-30具有更高的值。异常22-27的扩展速率为7.8 cm / yr,而异常27-30的扩展速率为10.3 cm / yr。异常30-33的传播速度为4.6厘米/年。另一个有趣的特征是,剖面在印度板块上的剖面上具有特征性的边缘效应异常,表明洋陆大陆壳边界。 [参考:31]

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