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Integrated Radiolarian and Conodont Biostratigraphy of the Middle to Late Permian Linghao Formation in Northwestern Guangxi, South China
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作者 ZHANG Lei WU Jun +9 位作者 YUAN Dongxun Marie Beatrice FOREL CHANG Shan Maliha Zareen KHAN FENG Qinglai HE Weihong MA Qiangfen Taniel DANELIAN Martial CARIDROIT Tsuyoshi ITO 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2021年第6期1984-1997,共14页
The Permian radiolarian zones and their correlations with conodont zones or other chronostratigraphic schemes are still under debate. In this study, four genera, 21 species and two subspecies of radiolarians together ... The Permian radiolarian zones and their correlations with conodont zones or other chronostratigraphic schemes are still under debate. In this study, four genera, 21 species and two subspecies of radiolarians together with one genus and six species of conodonts were recovered from the Linghao Formation cropping out at the Longwangpo(LWP) section, northwestern Guangxi, South China. Six radiolarian interval zones and one abundance zone are recognized in the section, namely in ascending order, the Follicucullus scholasticus, Albaillella cavitata, A. protolevis, A. levis, A. excelsa, A. triangularis Interval zones and A. yaoi Abundance Zone. They are correlated with the Clarkina dukouensis, C. guangyuanensis and C. orientalis conodont zones recognized at the same section. Based on our data, the F. scholasticus Interval Zone and the lowermost part of A. cavitata Interval Zone are recognized to be upper Capitanian age, whereas the four Albaillella Interval zones are of Lopingian age(Wuchiapingian to the late Changhsingian). Two previously known Changhsingian radiolarian zones, namely the A. triangularis and A. yaoi Interval zones, should be extended down to the uppermost Wuchiapingian in this studied section. 展开更多
关键词 biostratigraphy RADIOLARIA conodont elements Guadalupian/Capitanian–Lopingian linghao Formation GUANGXI
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贵州望谟纳夜领薅组上部遗迹化石特征及地质意义 被引量:1
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作者 向坤鹏 陈明华 +3 位作者 邓小杰 龙建喜 史振华 冉维宇 《贵州地质》 2021年第3期256-262,319,共8页
贵州望谟纳夜中-晚二叠世领薅组上部发育丰富的遗迹化石,主要识别出Chondrites,Planolites,Keckia及Helminthopsis等。含遗迹化石层段下部以Chondrites为优势化石种属,具有较高的丰度,向上逐渐被Planolites和Helminthopsis替代,整体形... 贵州望谟纳夜中-晚二叠世领薅组上部发育丰富的遗迹化石,主要识别出Chondrites,Planolites,Keckia及Helminthopsis等。含遗迹化石层段下部以Chondrites为优势化石种属,具有较高的丰度,向上逐渐被Planolites和Helminthopsis替代,整体形成以觅食迹为主的遗迹化石组合。根据领薅组上部岩石组合、沉积构造以及露头尺度遗迹化石的空间分布规律,结合区域地质资料综合分析认为:纳夜地区在中-晚二叠世整体为相对闭塞的浅海还原环境,遗迹化石是高水位体系沉积作用下的产物,其分布与海平面升降关系密切。化石组合的纵向变化规律指示向上水体整体变浅。这对于进一步认识贵州南部地区中-晚二叠世沉积演化提供了依据。 展开更多
关键词 遗迹化石 沉积构造 沉积环境 领薅组 纳夜地区
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