Tectonic or subsidence-induced movements

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SHAHBAZI ALIREZA; POURKHOSRAVANI MOHSEN

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Journal: QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES Year:2020 | Volume:8 | Issue:4 Page(s): 164-175

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Information Journal Paper

Title

Tectonic or subsidence-induced movements

Author(s)

SHAHBAZI ALIREZA | POURKHOSRAVANI MOHSEN | Issue Writer Certificate

Keywords

subsidenceQ2

DavalQ1

ShaqQ1

movementsQ1

Underground aquifersQ1

Abstract

In the last three decades, researchers have begun a wide-ranging effort to elucidate the causes of sedimentary cracks in the plains and have often attributed such gaps to excessive groundwater harvesting. Although subsidence in these plains has been proven credible by scientific documents, its relevance to water abstraction from Underground aquifers has been subject to some uncertainty, as the "shag" or "drum" phenomenon has been pre-empted by many Iranian peasants. The adoption of diesel suction technology and deep wells has been a well-known phenomenon. On the other hand, subsidence is not confined to low-negative plains and positive-low plains. This evidence led to the observation of the behavior of these plains in terms of water abstraction from aquifers and tectonic motions to clarify the cause of this issue by relying on different types of documents and empirical modeling of the underground in both dynamic and static conditions. The results of this study show that: * The phenomenon of drumming or drumming, which most scholars attribute to the overwhelming harvest of Underground aquifers, has a much longer historical history, so that this phenomenon before many diesel diggers and digging wells for many Iranian peasants. The phenomenon has been experienced and recognized. In the last three decades, researchers have begun a wide-ranging effort to elucidate the causes of sedimentary cracks in the plains and have often attributed such gaps to excessive groundwater harvesting. Although subsidence in these plains has been proven credible by scientific documents, its relevance to water abstraction from Underground aquifers has been subject to some uncertainty, as the "shag" or "drum" phenomenon has been pre-empted by many Iranian peasants. The adoption of diesel suction technology and deep wells has been a well-known phenomenon. On the other hand, subsidence is not confined to low-negative plains and positive-low plains. This evidence led to the observation of the behavior of these plains in terms of water abstraction from aquifers and tectonic motions to clarify the cause of this issue by relying on different types of documents and empirical modeling of the underground in both dynamic and static conditions. The results of this study show that: * The phenomenon of drumming or drumming, which most scholars attribute to the overwhelming harvest of Underground aquifers, has a much longer historical history, so that this phenomenon before many diesel diggers and digging wells for many Iranian peasants. The phenomenon has been experienced and recognized. In the last three decades, researchers have begun a wide-ranging effort to elucidate the causes of sedimentary cracks in the plains and have often attributed such gaps to excessive groundwater harvesting. Although subsidence in these plains has been proven credible by scientific documents, its relevance to water abstraction from Underground aquifers has been subject to some uncertainty, as the "shag" or "drum" phenomenon has been pre-empted by many Iranian peasants. The adoption of diesel suction technology and deep wells has been a well-known phenomenon. On the other hand, subsidence is not confined to low-negative plains and positive-low plains. This evidence led to the observation of the behavior of these plains in terms of water abstraction from aquifers and tectonic motions to clarify the cause of this issue by relying on different types of documents and empirical modeling of the underground in both dynamic and static conditions. The results of this study show that: * The phenomenon of drumming or drumming, which most scholars attribute to the overwhelming harvest of Underground aquifers, has a much longer historical history, so that this phenomenon before many diesel diggers and digging wells for many Iranian peasants. The phenomenon has been experienced and recognized. In the last three decades, researchers have begun a wide-ranging effort to elucidate the causes of sedimentary cracks in the plains and have often attributed such gaps to excessive groundwater harvesting. Although subsidence in these plains has been proven credible by scientific documents, its relevance to water abstraction from Underground aquifers has been subject to some uncertainty, as the "shag" or "drum" phenomenon has been pre-empted by many Iranian peasants. The adoption of diesel suction technology and deep wells has been a well-known phenomenon. On the other hand, subsidence is not confined to low-negative plains and positive-low plains. This evidence led to the observation of the behavior of these plains in terms of water abstraction from aquifers and tectonic motions to clarify the cause of this issue by relying on different types of documents and empirical modeling of the underground in both dynamic and static conditions. The results of this study show that: * The phenomenon of drumming or drumming, which most scholars attribute to the overwhelming harvest of Underground aquifers, has a much longer historical history, so that this phenomenon before many diesel diggers and digging wells for many Iranian peasants. The phenomenon has been experienced and recognized.

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APA: Copy

SHAHBAZI, ALIREZA, & POURKHOSRAVANI, MOHSEN. (2020). Tectonic or subsidence-induced movements. QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, 8(4 ), 164-175. SID. https://sid.ir/paper/379106/en

Vancouver: Copy

SHAHBAZI ALIREZA, POURKHOSRAVANI MOHSEN. Tectonic or subsidence-induced movements. QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES[Internet]. 2020;8(4 ):164-175. Available from: https://sid.ir/paper/379106/en

IEEE: Copy

ALIREZA SHAHBAZI, and MOHSEN POURKHOSRAVANI, “Tectonic or subsidence-induced movements,” QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, vol. 8, no. 4 , pp. 164–175, 2020, [Online]. Available: https://sid.ir/paper/379106/en

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