Decoding the Late Palaeozoic glaciated landscape of Namibia: A photogrammetric journey

IF 2.7 2区 地球科学 Q1 GEOLOGY Sedimentary Geology Pub Date : 2024-02-03 DOI:10.1016/j.sedgeo.2024.106592
D.P. Le Heron , C. Kettler , P. Dietrich , N. Griffis , I.P. Montañez , R. Wohlschlägl
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Abstract

The geometry of unconformities carved by deep time ice sheets is often obscured and restricted by discontinuous exposure, or outcrop conditions that do not readily permit the examination of glacial unconformities (for example, steeply dipping strata). Here, we present new uncrewed aerial vehicle (UAV) data from selected outcrops across northern, central and southern Namibia to shed further light on the nature of the basal Dwyka Group unconformity. This includes the onlap relationship of basal diamictites onto the Gomatum palaeo-fjord system in northern Namibia, highly complex mapped ice flow orientations elsewhere in the northern Kaokoveld, previously undiscovered grooves along the Fish River area, and a set of subglacial grooves along the border with South Africa along the Orange River. In the latter two cases, photogrammetric methods integrating orthophotos and digital elevation models reveal the presence of subglacial grooves. Furthermore, subglacial grooves often show different orientations to striations and fabrics measured in overlying diamictites, raising fresh questions about the nature of small-scale flow variations beneath Late Palaeozoic ice sheets.

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解密纳米比亚晚古生代冰川地貌:摄影测量之旅
由深时冰原雕刻而成的不整合地貌的几何形状往往因不连续的出露或不便于检查冰川不整合地貌的露头条件(例如,陡斜地层)而变得模糊不清和受到限制。在此,我们展示了来自纳米比亚北部、中部和南部部分露头的新的无人驾驶飞行器(UAV)数据,以进一步揭示基底 Dwyka 组不整合岩层的性质。这包括基底二迭石与纳米比亚北部戈马图姆古峡湾系统的重叠关系、考科维尔德北部其他地方高度复杂的冰流方向图、鱼河地区以前未发现的沟槽,以及沿奥兰治河与南非交界处的一组冰川下沟槽。在后两种情况下,综合正射影像和数字高程模型的摄影测量方法揭示了亚冰川沟槽的存在。此外,冰川下沟槽往往与在上覆二叠岩中测量到的纹理和结构显示出不同的方向,这就对晚古生代冰原下小规模流动变化的性质提出了新的问题。
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来源期刊
Sedimentary Geology
Sedimentary Geology 地学-地质学
CiteScore
5.10
自引率
7.10%
发文量
133
审稿时长
32 days
期刊介绍: Sedimentary Geology is a journal that rapidly publishes high quality, original research and review papers that cover all aspects of sediments and sedimentary rocks at all spatial and temporal scales. Submitted papers must make a significant contribution to the field of study and must place the research in a broad context, so that it is of interest to the diverse, international readership of the journal. Papers that are largely descriptive in nature, of limited scope or local geographical significance, or based on limited data will not be considered for publication.
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