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
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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。
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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.

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