马来西亚砂拉越Lubok Antu混杂岩中燧石块段的晚侏罗世至早白垩世放射虫

Basir Jasin
{"title":"马来西亚砂拉越Lubok Antu混杂岩中燧石块段的晚侏罗世至早白垩世放射虫","authors":"Basir Jasin","doi":"10.1016/0743-9547(96)00001-3","DOIUrl":null,"url":null,"abstract":"<div><p>The Lubok Antu melange is composed of blocks of mudstone, shale, sandstone, chert, limestone, hornfels, basalt, gabbro and serpentinite embedded in a strongly cleaved, pervasively sheared, chloritised mudstone matrix. Chert blocks are common and widespread in the melange. Fifty-three species of Radiolaria were identified from 14 samples collected from these chert blocks. The Radiolaria can be grouped into three assemblages. Assemblage I is composed of 17 species. The presence of <em>Ristola altissima</em> (Rüst) and <em>Parvicingula excelsa</em> Pessagno and Blome is indicative of late Tithonian (Late Jurassic). Assemblage II consists of 21 species. The occurrence of an index form <em>Staurosphaera septemporata</em> (Parona) indicates middle Valanginian to Barremian age. The presence of <em>Squinabollum fossilis</em> (Squinabol), <em>Archaeodictyomitra vulgaris</em> Pessagno, <em>Obesacapsula somphedia</em> (Foreman), <em>Thanarla praeveneta</em> Pessagno, <em>Pseudodictyomitra pseudomacrocephala</em> (Squinabol), <em>Rhopalosyringium majuroensis</em> Schaaf, <em>Stichomitra communis</em> Squinabol and <em>Holocryptocanium tuberculatum</em> Dumitrica in Assemblage III suggests that the age of this assemblage is late Albian to Cenomanian. All the results show that there are three different ages of the chert blocks present in the Lubok Antu melange.</p></div>","PeriodicalId":85022,"journal":{"name":"Journal of Southeast Asian earth sciences","volume":"13 1","pages":"Pages 1-11"},"PeriodicalIF":0.0000,"publicationDate":"1996-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0743-9547(96)00001-3","citationCount":"15","resultStr":"{\"title\":\"Late Jurassic to Early Cretaceous Radiolaria from chert blocks in the Lubok Antu melange, Sarawak, Malaysia\",\"authors\":\"Basir Jasin\",\"doi\":\"10.1016/0743-9547(96)00001-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The Lubok Antu melange is composed of blocks of mudstone, shale, sandstone, chert, limestone, hornfels, basalt, gabbro and serpentinite embedded in a strongly cleaved, pervasively sheared, chloritised mudstone matrix. Chert blocks are common and widespread in the melange. Fifty-three species of Radiolaria were identified from 14 samples collected from these chert blocks. The Radiolaria can be grouped into three assemblages. Assemblage I is composed of 17 species. The presence of <em>Ristola altissima</em> (Rüst) and <em>Parvicingula excelsa</em> Pessagno and Blome is indicative of late Tithonian (Late Jurassic). Assemblage II consists of 21 species. The occurrence of an index form <em>Staurosphaera septemporata</em> (Parona) indicates middle Valanginian to Barremian age. The presence of <em>Squinabollum fossilis</em> (Squinabol), <em>Archaeodictyomitra vulgaris</em> Pessagno, <em>Obesacapsula somphedia</em> (Foreman), <em>Thanarla praeveneta</em> Pessagno, <em>Pseudodictyomitra pseudomacrocephala</em> (Squinabol), <em>Rhopalosyringium majuroensis</em> Schaaf, <em>Stichomitra communis</em> Squinabol and <em>Holocryptocanium tuberculatum</em> Dumitrica in Assemblage III suggests that the age of this assemblage is late Albian to Cenomanian. All the results show that there are three different ages of the chert blocks present in the Lubok Antu melange.</p></div>\",\"PeriodicalId\":85022,\"journal\":{\"name\":\"Journal of Southeast Asian earth sciences\",\"volume\":\"13 1\",\"pages\":\"Pages 1-11\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1996-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0743-9547(96)00001-3\",\"citationCount\":\"15\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Southeast Asian earth sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0743954796000013\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Southeast Asian earth sciences","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0743954796000013","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 15

摘要

Lubok-Antu混杂岩由泥岩、页岩、砂岩、燧石、石灰岩、角砾岩、玄武岩、辉长岩和蛇纹岩块组成,嵌入强烈解理、普遍剪切、氯化的泥岩基质中。燧石块体在混杂岩中普遍存在。从这些燧石块采集的14个样本中鉴定出53种放射虫。放射虫可分为三个组合。总集I由17个种组成。Ristola altissima(Rüst)和Parvicingula excelsa Pessagno和Blome的存在表明了提香阶晚期(侏罗纪晚期)。集合II由21个物种组成。一个指数型七分球藻(Parona)的出现表明瓦朗吉安中期至巴雷米安期。Squinabollum化石(Squinabol)、Archeodictyomitra vulgaris Pessagno、Obesacapsula somphedia(Foreman,Stichomitra commons Squinabol和Holocryptocanium tuberculatum Dumitrica在Assemblage III中表明,该组合的年龄为阿尔布晚期至塞诺曼期。结果表明,鲁博克-安图混杂岩中存在三个不同时代的燧石块体。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Late Jurassic to Early Cretaceous Radiolaria from chert blocks in the Lubok Antu melange, Sarawak, Malaysia

The Lubok Antu melange is composed of blocks of mudstone, shale, sandstone, chert, limestone, hornfels, basalt, gabbro and serpentinite embedded in a strongly cleaved, pervasively sheared, chloritised mudstone matrix. Chert blocks are common and widespread in the melange. Fifty-three species of Radiolaria were identified from 14 samples collected from these chert blocks. The Radiolaria can be grouped into three assemblages. Assemblage I is composed of 17 species. The presence of Ristola altissima (Rüst) and Parvicingula excelsa Pessagno and Blome is indicative of late Tithonian (Late Jurassic). Assemblage II consists of 21 species. The occurrence of an index form Staurosphaera septemporata (Parona) indicates middle Valanginian to Barremian age. The presence of Squinabollum fossilis (Squinabol), Archaeodictyomitra vulgaris Pessagno, Obesacapsula somphedia (Foreman), Thanarla praeveneta Pessagno, Pseudodictyomitra pseudomacrocephala (Squinabol), Rhopalosyringium majuroensis Schaaf, Stichomitra communis Squinabol and Holocryptocanium tuberculatum Dumitrica in Assemblage III suggests that the age of this assemblage is late Albian to Cenomanian. All the results show that there are three different ages of the chert blocks present in the Lubok Antu melange.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信