Folding of Oceanic Crust Along the Davie Fracture Zone, Offshore Tanzania Article Swipe
Xi Peng
,
Yuanyuan Zhou
,
Wang Li
,
Zhaoqian Liu
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3390/jmse13061179
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3390/jmse13061179
The Davie Fracture Zone (Davie FZ)—among the longest offshore transform systems in East Africa—mediated Madagascar’s southward displacement following Gondwana’s Early Jurassic breakup. This giant structure has a distinct topography and gravity field signals. However, it is buried by thick sediments in its northern segment offshore Tanzania, hindering understanding of the internal structures and their origin. In this study, we applied 2-D multichannel seismic to analyze the structural characteristics and evolution of the Davie FZ. The Davie FZ is located in the oceanic domain, which is bordered by the landwards-dipping overthrust fault at the continent–ocean boundary. Volcano sediments atop the basement with undulating Moho reflection below depict a typical oceanic domain. Distinct compressive deformation characterized by the crustal undulation of around 40 km wavelength forms folded oceanic crust, and Late Jurassic sediments onlap onto the crest of the folded basement. The Davie FZ is localized in a corridor with the thickened oceanic crust and is presented by positive flower structures with faulted uplifted basement and deepened Moho. The Davie FZ evolved from a proto-transform fault located in Gondwana before the spreading of the West Somali Basin. During the Late Jurassic, a kinematic change shifted the spreading direction from NW–SE to N–S, resulting in a strike-slip of the Davie FZ and contemporaneous transpressional deformation offshore Tanzania. The Davie FZ is an excellent case to understand the tectonic-magmatic process forming this transform margin.
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Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.3390/jmse13061179
- https://www.mdpi.com/2077-1312/13/6/1179/pdf?version=1750151174
- OA Status
- gold
- References
- 55
- Related Works
- 10
- OpenAlex ID
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All OpenAlex metadata
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https://openalex.org/W4411338400Canonical identifier for this work in OpenAlex
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https://doi.org/10.3390/jmse13061179Digital Object Identifier
- Title
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Folding of Oceanic Crust Along the Davie Fracture Zone, Offshore TanzaniaWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2025Year of publication
- Publication date
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2025-06-16Full publication date if available
- Authors
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Xi Peng, Yuanyuan Zhou, Wang Li, Zhaoqian LiuList of authors in order
- Landing page
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https://doi.org/10.3390/jmse13061179Publisher landing page
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https://www.mdpi.com/2077-1312/13/6/1179/pdf?version=1750151174Direct link to full text PDF
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://www.mdpi.com/2077-1312/13/6/1179/pdf?version=1750151174Direct OA link when available
- Concepts
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Tanzania, Submarine pipeline, Geology, Oceanic crust, Crust, Oceanography, Seismology, Folding (DSP implementation), Subduction, Paleontology, Geography, Tectonics, Electrical engineering, Environmental planning, EngineeringTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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| publication_date | 2025-06-16 |
| publication_year | 2025 |
| referenced_works | https://openalex.org/W2009786134, https://openalex.org/W1968534064, https://openalex.org/W2074593631, https://openalex.org/W4200500967, https://openalex.org/W4288070723, https://openalex.org/W4391145541, https://openalex.org/W2121329342, https://openalex.org/W2171056591, https://openalex.org/W2142803987, https://openalex.org/W1998437836, https://openalex.org/W2013895795, https://openalex.org/W2063196787, https://openalex.org/W1998171101, https://openalex.org/W1853607249, https://openalex.org/W2559471396, https://openalex.org/W2791215467, https://openalex.org/W4200317247, https://openalex.org/W4210636680, https://openalex.org/W3210815043, https://openalex.org/W4212902128, https://openalex.org/W1963735255, https://openalex.org/W2067886668, https://openalex.org/W3155937730, https://openalex.org/W2913753229, https://openalex.org/W2294794500, https://openalex.org/W2333512730, https://openalex.org/W2025049414, https://openalex.org/W2921914663, https://openalex.org/W2336433913, https://openalex.org/W4297474496, https://openalex.org/W3161716668, https://openalex.org/W2562655409, https://openalex.org/W2971486618, https://openalex.org/W2339480430, https://openalex.org/W1997442805, https://openalex.org/W2178484906, https://openalex.org/W2105360073, https://openalex.org/W2003134995, https://openalex.org/W2074021412, https://openalex.org/W2017995563, https://openalex.org/W3004878113, https://openalex.org/W1998589072, https://openalex.org/W2159221900, https://openalex.org/W1907977727, https://openalex.org/W2025841258, https://openalex.org/W2768451290, https://openalex.org/W1998395901, https://openalex.org/W2902722557, https://openalex.org/W2153793888, https://openalex.org/W2047478481, https://openalex.org/W2799565698, https://openalex.org/W6796208938, https://openalex.org/W2010727548, https://openalex.org/W1971154511, https://openalex.org/W2034011749 |
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