Correlation of Paleo-Mesozoic Sandstones Based on Heavy Mineral Chemistry and Th–U–Total Pb Monazite Dating: Implications on Paleogeographic Reconstruction in Eastern Gondwanaland

IF 2.2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2026-04-09 Epub Date: 2025-06-27 DOI:10.1002/gj.70023
Sankar Kumar Nahak, Sanghita Dasgupta, N. Prabhakar, Santanu Banerjee
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引用次数: 0

Abstract

The correlation between continental sandstones in adjacent sedimentary basins, lacking biostratigraphic control, is often problematic. Based on petrography, paleocurrent data, heavy mineral analysis, and monazite dating, this study correlates Paleo-Mesozoic sandstones in the Wardha Basin with those in the adjacent Pranhita-Godavari (P-G) Basin, and presents a paleogeographic reconstruction of eastern Gondwanaland. Predominantly quartzose to feldspathic-quartzose arenites of the Wardha Basin, showing N-NW paleocurrent, contain heavy minerals such as ilmenite, garnet, zircon, rutile, monazite, tourmaline, and staurolite. Burial dissolution has caused preferential leaching of staurolite and rutile in relatively older sediments. The abundance of almandine garnet indicates the predominant granulite and subordinate amphibolite sources. The tourmaline chemistry, indicating the dominance of dravite and schorl, relates them primarily to amphibolites and granitoids, whilst rutile chemistry tracks them to metapelitic sources. The prevalence of leucoxene in younger formations reflects ilmenite alteration, indicating progressive tectonic stability and humidity from the Upper Carboniferous to Lower Triassic period. The Th–U–total Pb dating of detrital monazite in sandstones yields three major groups at (1) 2496–2395 Ma, (2) 927–722 Ma, and (3) 552–438 Ma. Heavy mineral chemistry, paleocurrent data, and monazite dating track sediment sources to the Eastern Ghats Mobile Belt, Karimnagar Granulite Belt, and Antarctica through the axial drainage system. Whilst local sediment sources include amphibolites and granitoids in Bastar Craton, hosting Bhopalpatnam Granulite Belt, Mul and Dongargarh granite, and Bengpal Group. Good matching of heavy mineral chemistry and monazite dating confirms the genetic relationship between Wardha Basin and Pranhita-Godavari Basin.

Abstract Image

古中生代砂岩重矿物化学对比与th - u -总Pb独居石定年:对冈瓦纳大陆东部古地理重建的启示
由于缺乏生物地层控制,相邻沉积盆地中陆相砂岩的对比往往存在问题。根据岩石学、古流学、重矿物分析和独居石定年等资料,将瓦尔达盆地的古中生代砂岩与邻近的Pranhita-Godavari (P-G)盆地进行对比,重建了冈瓦纳兰东部的古地理。瓦尔达盆地以石英-长石-石英砂岩为主,古海流为N-NW,含钛铁矿、石榴石、锆石、金红石、独居石、电气石、橄榄石等重矿物。埋藏溶蚀作用在相对较老的沉积物中造成了优先浸出的锆石和金红石。石榴石丰度表明麻粒岩为主,角闪岩次之。电气石的化学特征表明其主要来源于闪长岩和花岗岩,而金红石的化学特征则表明其主要来源于变质长岩。较年轻地层中亮新世的盛行反映了钛铁矿蚀变,表明上石炭统至下三叠统的构造稳定性和湿度渐进性。砂岩碎屑独居石的Th-U-total Pb定年分为(1)2496 ~ 2395 Ma、(2)927 ~ 722 Ma和(3)552 ~ 438 Ma三大类。通过轴向排水系统,重矿物化学、古流数据和独居石定年追踪了东高止山脉移动带、卡里姆纳格尔麻粒岩带和南极洲的沉积物来源。而在Bastar克拉通,沉积源主要为角闪岩和花岗岩类,含Bhopalpatnam麻粒岩带、Mul和Dongargarh花岗岩和Bengpal群。重矿物化学和独居石定年的良好匹配证实了瓦尔达盆地与普拉纳希塔-戈达瓦里盆地的成因关系。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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