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    <link>http://pucir.inflibnet.ac.in:8080/jspui/handle/123456789/588</link>
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    <pubDate>Wed, 29 Apr 2026 11:22:08 GMT</pubDate>
    <dc:date>2026-04-29T11:22:08Z</dc:date>
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      <title>CORRELATION OF FOUR MAGNETOSTRATIGRAPHICALLY CONSTRAINED SECTIONS OF MIOCENE BHUBAN FORMATION OF SURMA BASIN IN MIZORAM, INDIA</title>
      <link>http://pucir.inflibnet.ac.in:8080/jspui/handle/123456789/589</link>
      <description>Title: CORRELATION OF FOUR MAGNETOSTRATIGRAPHICALLY CONSTRAINED SECTIONS OF MIOCENE BHUBAN FORMATION OF SURMA BASIN IN MIZORAM, INDIA
Authors: Lalremruatfela, C
Abstract: In the present study, four magnetostratigraphically constrained isolated sections in the Mizoram part of the Surma basin, namely,&#xD;
Kolasib-Rengtekawn (KR) section in Kolasib district; and Bawngkawn–Durtlang (BD); Tuirial and Sairang sections in Aizawl district of&#xD;
Mizoram have been successfully correlated. The youngest magnetozone of BD section i. e. C5Cn magnetozone (16.726-16.014 Ma) has&#xD;
also been recorded in the KR section and both the sections expose Middle Bhuban Unit of Bhuban Formation, Surma Group. Thus KR&#xD;
section is correlated with the upper part of BD section. Three younger magnetozones, viz., C4 An (9.025 - 8.699 Ma), C4Ar.1n (9.308 -&#xD;
9.230 Ma) and C4Ar.2n (9.642 - 9.580 Ma) of Tuirial section have been delineated in the Sairang section and both the sections belong to&#xD;
Upper Bhuban Unit. Thus Sairang section is correlatable with the upper part of Tuirial section. Stratigraphically also, KR and BD sections&#xD;
are older than the Tuirial and Sairang sections. Similar pattern in rate of deposition has been noticed in the KR and BD sections and Turial&#xD;
and Sairang sections. The study thus demonstrates that magnetostratigraphy may emerge as the reliable tool for regional correlation of&#xD;
isolated successions of varied litho-stratigraphic units in the Surma basin. An integrated study on litho-, bio- and magnetostratigraphy along&#xD;
with sedimentology is needed to reconstruct the tectono-depositional history of the basin and biotic evolution in it.</description>
      <pubDate>Sat, 01 Feb 2014 00:00:00 GMT</pubDate>
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      <dc:date>2014-02-01T00:00:00Z</dc:date>
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