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Reconciling plate motion and faulting at a rift-rift-rift triple junction

Urheber*innen

Maestrelli,  Daniele
External Organizations;

Sani,  Federico
External Organizations;

Keir,  Derek
External Organizations;

Pagli,  Carolina
External Organizations;

La Rosa,  Alessandro
External Organizations;

/persons/resource/ameha

Muluneh,  Ameha A.
2.5 Geodynamic Modelling, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/brune

Brune,  Sascha
2.5 Geodynamic Modelling, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Corti,  Giacomo
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Zitation

Maestrelli, D., Sani, F., Keir, D., Pagli, C., La Rosa, A., Muluneh, A. A., Brune, S., Corti, G. (2024): Reconciling plate motion and faulting at a rift-rift-rift triple junction. - Geology, 52, 5, 362-366.
https://doi.org/10.1130/G51909.1


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5025407
Zusammenfassung
Rift-Rift-Rift triple junctions are regions where three plates interact, generating complex networks of variably oriented faults. While the geometry of the fault networks is easily constrained from their surface expression, what remains unclear is how the kinematics of faults and their interactions vary spatially, and how these relate to the unusual crustal motions that result from three plates diverging from each other. The Afar depression lies at the triple junction between the African, Arabian, and Somalian plates (in the Horn of Africa), where the unique combination of observational data from structural mapping, seismicity, and Global Navigation Satellite System (GNSS) allows us to understand the link between fault kinematics and plate motions. We complement these observations with an analog model to gain insights into how the patterns and directions of faults relate to overall plate motions. A key finding in both the model and nature is that some adjacent normal faults form at high angles and generate T-shaped structures. These purely normal faults are synchronously active, which means that the extension direction varies ∼90° locally. These kinematic contrasts in our model and in nature occur despite the relatively smooth pattern of overall surface motions. The results indicate that normal faults interacting at high angles to form the T-shaped structures can evolve synchronously within a stress field that varies gently in magnitude but dramatically in orientation over a few kilometers.