Anisotropy of magnetic susceptibility and rock magnetism of high-grade rocks from Eastern Ghats Mobile Belt, India: Constraints to tectonics

IF 1.3 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Journal of Earth System Science Pub Date : 2024-09-02 DOI:10.1007/s12040-024-02397-x
Solanky Das, M Venkateshwarlu, Supriya Mondal, Saurodeep Chatterjee, Debesh Gain
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Abstract

The present study deals with the Fe–Ti oxides, rock magnetic and anisotropy of magnetic susceptibility (AMS) carried out to determine the magneto-mineralogical characteristics and the nature of the magnetic fabrics of the high-grade metamorphic rocks from Chilka Lake area, Eastern Ghats Mobile Belt (EGMB), India. Petrography depicted the presence of both primary and secondary magnetite and titano-magnetite as the chief magnetic minerals. Different generations of magnetite were found in these rocks corresponding to different conditions of temperature that prevailed during their oxidation, having tectonic implications depicting the crustal upliftment. Thermomagnetic analysis, isothermal remanent magnetization (IRM), hysteresis loops and backfield IRM demagnetisation show the presence of ferrimagnetic minerals of different origin. The magnetic domain is determined by Day plot, using the remanence and coercivity values from hysteresis curves, dominated by stable single domain (SSD), which reveals the potentiality to record the ancient magnetic field. AMS studies unravelled the nature of the magnetic fabrics in the region. The magnetic susceptibility ellipsoids are dominantly oblate as revealed from the PjTj shape plots. The magnetic lineation is highly variable which states the multiple phased tectono-metamorphic conditions. The similarity between the magnetic and mesoscopic fabrics in the granulite is significant, whereas the anorthosites result from felsic magmatism, which occurred after the deformational phases and thus did not record any mesoscopic tectonic significance.

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印度东高止山脉移动带高品位岩石的磁感应强度和岩石磁性各向异性:构造的制约因素
本研究涉及铁钛氧化物、岩石磁性和磁感应强度各向异性(AMS),目的是确定印度东高止山脉移动带 Chilka 湖地区高品位变质岩的磁矿物学特征和磁结构性质。岩相学描述了主要磁性矿物原生磁铁矿、次生磁铁矿和钛磁铁矿的存在。在这些岩石中发现了不同世代的磁铁矿,与岩石氧化过程中的不同温度条件相对应,具有描述地壳隆起的构造影响。热磁分析、等温剩磁(IRM)、磁滞回线和后场 IRM 退磁显示了不同来源的铁磁性矿物的存在。利用磁滞曲线中的剩磁和矫顽力值,通过戴氏图确定了磁畴,其中以稳定单磁畴(SSD)为主,揭示了记录古磁场的潜力。AMS 研究揭示了该地区磁结构的性质。Pj-Tj 形状图显示,磁感应强度椭球体主要呈扁圆形。磁力线的变化很大,说明了多期构造-变质条件。花岗岩中的磁性构造与中观构造之间具有显著的相似性,而正长岩则是在变形阶段之后发生的长纤维岩浆作用的结果,因此不具有任何中观构造意义。
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来源期刊
Journal of Earth System Science
Journal of Earth System Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
3.20
自引率
5.30%
发文量
226
期刊介绍: The Journal of Earth System Science, an International Journal, was earlier a part of the Proceedings of the Indian Academy of Sciences – Section A begun in 1934, and later split in 1978 into theme journals. This journal was published as Proceedings – Earth and Planetary Sciences since 1978, and in 2005 was renamed ‘Journal of Earth System Science’. The journal is highly inter-disciplinary and publishes scholarly research – new data, ideas, and conceptual advances – in Earth System Science. The focus is on the evolution of the Earth as a system: manuscripts describing changes of anthropogenic origin in a limited region are not considered unless they go beyond describing the changes to include an analysis of earth-system processes. The journal''s scope includes the solid earth (geosphere), the atmosphere, the hydrosphere (including cryosphere), and the biosphere; it also addresses related aspects of planetary and space sciences. Contributions pertaining to the Indian sub- continent and the surrounding Indian-Ocean region are particularly welcome. Given that a large number of manuscripts report either observations or model results for a limited domain, manuscripts intended for publication in JESS are expected to fulfill at least one of the following three criteria. The data should be of relevance and should be of statistically significant size and from a region from where such data are sparse. If the data are from a well-sampled region, the data size should be considerable and advance our knowledge of the region. A model study is carried out to explain observations reported either in the same manuscript or in the literature. The analysis, whether of data or with models, is novel and the inferences advance the current knowledge.
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