Integrating pseudo-3D ERT and DEM to map the near-surface structures and morphology of the Piparo mud volcano, Trinidad

Blake, O. O.; Ramsook, Ryan; Iyare, U. C.; Moonan, Xavier; Gopaul, R.C.

doi:10.1016/j.jappgeo.2021.104442

Cited by 5 publications

(3 citation statements)

References 32 publications

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“…The geoelectrical data in [19], also from the Pâclele Mici volcano, suggest somewhat lower values. This is challenging because high conductivity [20] is often associated with reduced contrast, higher attenuation, and challenges in data interpretation. As geoelectrical surveys rely on the propagation of electrical currents through the subsurface, high conductive subsurface materials allow easy flow of these currents but also quickly dissipate the electrical energy.…”

Section: Study Sitementioning

confidence: 99%

A Geophysical Investigation of the Pâclele Mici Mud Volcano in Romania Using Deep Geoelectrical Surveys

Mihai,

Gerea,

Tataru

et al. 2024

Applied Sciences

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This work presents a case study of a geoelectrical exploration of understudied mud volcanoes in Romania, specifically the Pâclele Mici mud volcano from Buzău County. Using a geoelectrical technique facilitated by the distributed network of V-FullWaver equipment, we present, to our knowledge, the first deep 3D case study of a mud volcano in the country. The findings indicate that while geoelectrical surveys in such environments are met with important challenges in terms of soil conductivity, they nonetheless provide a viable approach to uncovering the complex structures and processes of mud volcanoes. We map a part of the mud volcano, showing that the active subsurface part corresponds only partly with what is visible on the surface, and suggest a framework for an in-depth analysis of the extensive mud volcano area.

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Section: Study Sitementioning

confidence: 99%

A Geophysical Investigation of the Pâclele Mici Mud Volcano in Romania Using Deep Geoelectrical Surveys

Mihai,

Gerea,

Tataru

et al. 2024

Applied Sciences

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“…Resistivity methods have also been used to identify the underground structure of mud volcanic layers. According to a study by [13], [14], a resistivity tool (Pseudo3D ERT) combined with a digital elevation model (DEM) can characterize the underground structure of Piparomad Mountain in Trinidad and Tobago. The results showed a low resistivity value (<2.5 ohm.m) in the Mud Volcano sediment flows in the main vent.…”

Section: Fig 2 Wenner-schlumberger Configurationmentioning

confidence: 99%

Electrical Resistivity Survey of the Gunung Anyar Mud Volcano

Wardhani

Aryaseta²,

Puspitasari³

2022

JACEE

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The past oil and natural gas drilling activities have been presumed to cause a Mud Volcano phenomenon. The Mud Volcano potentially danger its surroundings, including the inhabitants. Thus, mapping the zone will be essential to have a mitigation plan. One of the potential Mud Volcanoes is the Gunung Anyar Mud Volcano. By using a resistivity survey, this research aims to obtain the subsurface structure of the Gunung Anyar Mud Volcano. The results show that very low resistivity values are located at the top of the soil structure with 0 to 4 meters depth. This soil structure is believed to be a manifestation of a mud volcano in the form of moistened clay associated with salt water. At subsequent depths, 4 to 5.5 meters from the top, is a layer of sandy clay. It is characterized by moderate to high resistivity values. At a depth of 5.5 to 10.5 meters, the resistivity value is very high. This sandstone layer is most likely a native subsoil formation in the Gunung Anyar area.

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“…To date, mud volcanic hazard is underestimated as shown by recent mud eruptions. In 1997 the eruption of the Piparo mud volcano (Island of Trinidad) buried roads and houses, damaged electrical and water infrastructures and killed animals and livestock (Blake et al., 2021). In 2014, the violent and unexpected eruption of the Macalube di Aragona mud volcano, (Italy) caused two fatalities (Gattuso et al., 2021; Napoli et al., 2020).…”

Section: Introductionmentioning

confidence: 99%

Gravity Data Allow to Image the Shallow‐Medium Subsurface Below Mud Volcanoes

Nespoli,

Antonellini,

Albarello

et al. 2023

Geophysical Research Letters

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The debate about the conceptual model of mud volcanoes functioning is still alive in the literature. A large part of the literature focuses on the characterization of the deep reservoir where expelled fluids are expected to originate. Another part of literature is focused on the study of the shallow system of mud volcanoes, which could influence the short‐term variations in mud volcanoes activity. We present and analyze a new data set of micro‐gravimetric data to study the area of the Nirano Salse, Italy. Unlike what is commonly assumed for the study area, our results suggest that the geomorphology of the Nirano Salse is not related to a caldera collapse above a shallow mud chamber, but to the surface expression of slip distribution of a fault termination along which the fluids ascended to the surface. We believe that gravimetric data can significantly improve the study of hydrocarbon seeps and mud volcanism.

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Integrating pseudo-3D ERT and DEM to map the near-surface structures and morphology of the Piparo mud volcano, Trinidad

Cited by 5 publications

References 32 publications

A Geophysical Investigation of the Pâclele Mici Mud Volcano in Romania Using Deep Geoelectrical Surveys

A Geophysical Investigation of the Pâclele Mici Mud Volcano in Romania Using Deep Geoelectrical Surveys

Electrical Resistivity Survey of the Gunung Anyar Mud Volcano

Gravity Data Allow to Image the Shallow‐Medium Subsurface Below Mud Volcanoes

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