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海南岛西部大广坝地区晚奥陶世-早志留世笔石地层的发现及意义

龙文国 周岱 王晶 柯贤忠 周建波 汪焰华

华南地质与矿产2016,Vol.32Issue(1):10-14,5.
华南地质与矿产2016,Vol.32Issue(1):10-14,5.DOI:10.3969/j.issn.1007-3701.2016.01.002

海南岛西部大广坝地区晚奥陶世-早志留世笔石地层的发现及意义

Discovery of Late Ordovician- Early Silurian graptolites and its Significance in Daguangba area of Hainan Island.

龙文国 1周岱 2王晶 1柯贤忠 2周建波 1汪焰华2

作者信息

  • 1. 中国地质调查局武汉地质调查中心,武汉430205
  • 2. 中国地质调查局花岗岩成岩成矿地质研究中心,武汉430205
  • 折叠

摘要

Abstract

The Ordovician-Silurian graptolites, which were identified as diplograptid, were firstly discovered in light-metamorphosed rock series in Daguangba in western Hainan Island. However, there was long-term de-bate on the age of the light metamorphic strata, it has been regarded as the Cambrian, Pre-Devonian, Devoni-an-Carboniferous, Carboniferous and Permian. The discovery of the graptolite fossils not only offered new evi-dences for the age of the fosils-bearing strata and further confirmed the occurrence of the late Ordovician to early Silurian strata in central-north Hainan Island, but also for Ordovician-Silurian stratigraphic division and correlation of the deep-water facies, and playing important roles in the research on paleobiogeographic provincialization, sedimentary facies and sedimentary tectonic background of Hainan Island and adjacent area.

关键词

笔石/晚奥陶世-早志留世/沉积相/大广坝/海南岛

Key words

graptolite/Late Ordovician-Early Silurian/sedimentary facies/Daguangba, Hainan Island

分类

地质学

引用本文复制引用

龙文国,周岱,王晶,柯贤忠,周建波,汪焰华..海南岛西部大广坝地区晚奥陶世-早志留世笔石地层的发现及意义[J].华南地质与矿产,2016,32(1):10-14,5.

基金项目

中国地质调查局项目“钦杭西段关键地区区域地质调查(12120113066400)”和国家自然基金项目“广西泥盆纪双壳动物系统古生物学及多样性演变(41172025)”资助 ()

华南地质与矿产

1007-3701

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