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ABSTRACT There have been growing needs for scientists to search for efficiently high-resolution geophysical techniques to image the subsurface features, formations, and shallow geologic structures (e.g. faults, void, stratigraphy features). At shallow depths, an in-depth understanding of these features/structures could be pivotal in in the management of the environment and crucial examination of hazardous terrains which are of growing threat to human safety. In the case of Malta, with a limited land space, their study could be relevant to the environmental planning agency in advocating for safe building sites for structural architecture as well as use of land. In this regard, this study will be investigating such features located in Malta, one in the Selmun Promontory, locatedin the north-eastern zone, and the second in the Mellieha valley located in the north-western zone of the Maltese archipelago. On the Selmun area ERTs arrays and passive seismic measurements were recorded both in the slope and on the plateau. Results are interpreted in terms of geological stratigraphy and whether zones on the plateau were identified, where rock falls and other slope processes are incipient. In the Mellieha Area, ERTs arrays, GPR scans and ambient noise measurements indicate the presence of unmapped fault zonesand sediment distribution, improving the understanding of the local geology.
Iregbeyen et al. (Fri,) studied this question.
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