The Connection Between Okavango (Botswana) and Kafue (Zambia) Rift Zone from Satellite Gravity and Aeromagnetic Data: Implication for the Evolution of the Southwestern Branch of the East African Rift System

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Farjana Mily, Luelseged Emishaw, Andrew Katumwehe, Kevin Mickus, Mohamed Abdelsalam
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Abstract

We analyzed gravity and magnetic data to investigate the lithospheric connection between the Okavango Rift Zone (ORZ) in northwestern Botswana and the Kafue Rift Zone (KRZ) in Zambia. The tectonic environment and the lithospheric structure of the ORZ is well understood, the lithospheric structure of the KRZ and surrounding region is basically unknown. Determining this lithospheric structure and how or if the ORZ and KRZ are tectonically related, a gravity and magnetic data analysis using a power spectrum analysis combined with the two-dimensional gravity forward models constrained by seismic data was conducted. The gravity power spectrum analysis indicated that the crust was thinned by between 4 and 5 km beneath both rift zones compared to the surrounding Proterozoic terranes, with the depth to the Mid Crustal Discontinuity (MCD) thinned by 2–3 km. Additionally, the gravity models suggested that the region between the ORZ and KRZ exhibits a shallower depths to the Moho and MCD, which implies that rifting process is an ongoing process that links these rift zones A derivative analysis of the aeromagnetic data analysis indicated that the fabric of the Proterozoic crystalline basement structures aligns parallel to the ORZ and the power spectrum analysis that showed that the depth to basement within the transfer zones between the basins were deeper, implying that the basins are tectonically linked. The basement fabric is perpendicular to the KRZ which implies that the ORZ was formed in a structurally weak zone between the Congo and Kalahari Cratons and that block rotation within the KRZ region facilitated the extension that formed the rift. Though there is age difference between the ORZ and KRZ, the connectivity of the two rift zones indicates that there is a continuation of the Western Branch of the East African Rift System from Zambia into Botswana.

从卫星重磁资料看博茨瓦纳奥卡万戈和赞比亚Kafue裂谷带的联系:对东非裂谷系西南分支演化的启示
为了研究博茨瓦纳西北部奥卡万戈裂谷带(ORZ)与赞比亚Kafue裂谷带(KRZ)之间的岩石圈联系,我们分析了重磁资料。对ORZ的构造环境和岩石圈结构有较好的认识,对KRZ及周边地区的岩石圈结构基本未知。为了确定该岩石圈结构以及ORZ和KRZ是否存在构造上的联系,利用功率谱分析结合地震数据约束下的二维重力正演模型对重磁数据进行了分析。重力功率谱分析表明,两个裂谷带下的地壳与周围元古代地体相比变薄了4 ~ 5 km,到中地壳不连续面(MCD)的深度变薄了2 ~ 3 km。此外,重力模型表明ORZ和KRZ之间的区域比Moho和MCD的深度更浅。航磁资料的导数分析表明,元古代结晶基底结构与ORZ平行,功率谱分析表明,盆地间转移带的基底深度更深,表明盆地之间存在构造联系。基底构造垂直于KRZ,这表明ORZ形成于刚果克拉通和喀拉哈里克拉通之间的构造薄弱地带,而KRZ区域内的地块旋转促进了裂谷的伸展形成。尽管ORZ和KRZ之间存在年龄差异,但两个裂谷带的连通性表明,东非裂谷系西部分支从赞比亚延伸到博茨瓦纳。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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