2020
DOI: 10.1007/s12517-020-5122-5
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Structural styles, hydrocarbon prospects, and potential of Miano and Kadanwari fields, Central Indus Basin, Pakistan

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Cited by 7 publications
(1 citation statement)
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“…The occurrence of ophiolites on the western slope of this belt suggests the existence of an active plate boundary in the past, which is further confirmed by seismic activity. Mafic to ultramafic rocks are the dominant rock types along this active plate boundary, according to Jadoon et al [17]. The region being studied, located south of the Central Indus Basin (Figure 1), contains preexisting normal faults oriented in a NW-SE direction that runs parallel to the Jacobabad highs and disrupts the foredeep region.…”
Section: Tectonics Geology and Stratigraphy Of The Study Areamentioning
confidence: 86%
“…The occurrence of ophiolites on the western slope of this belt suggests the existence of an active plate boundary in the past, which is further confirmed by seismic activity. Mafic to ultramafic rocks are the dominant rock types along this active plate boundary, according to Jadoon et al [17]. The region being studied, located south of the Central Indus Basin (Figure 1), contains preexisting normal faults oriented in a NW-SE direction that runs parallel to the Jacobabad highs and disrupts the foredeep region.…”
Section: Tectonics Geology and Stratigraphy Of The Study Areamentioning
confidence: 86%