QUANTITATIVE ANALYSIS OF TECTONIC ACTIVITY IN TAFTAN VOLCANO AND AROUND (SOUTH EAST OF IRAN)

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JAMI MOHSEN; SALGI ALI; POORKERMANI MOHSEN; MORIDI FARIMANI ALI ASGHAR

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Journal: JOURNAL OF NATURAL ENVIRONMENT HAZARDS Year:2017 | Volume:5 | Issue:10 Page(s): 117-144

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Title

QUANTITATIVE ANALYSIS OF TECTONIC ACTIVITY IN TAFTAN VOLCANO AND AROUND (SOUTH EAST OF IRAN)

Author(s)

JAMI MOHSEN | SALGI ALI | POORKERMANI MOHSEN | MORIDI FARIMANI ALI ASGHAR | Issue Writer Certificate

Keywords

ACTIVE TECTONICSQ1

VOLCANO TAFTANQ2

MORPHOMETRIC PARAMETERSQ1

SARAVAN FAULTQ1

Abstract

Taftan volcano young to age Pliocene-Quaternary and a semi-active volcanic system is located 50 kilometers north of the city of Khash. According to population centers around the volcano and the earthquake of high magnitude in this area (earthquakes related to SARAVAN FAULT), study tectonic activity in this area is important. In the field of geomorphic indicators, it has been used for the study of tectonic activity. These indicators include the drainage basin asymmetry (Af), mountain front sinuosity (Smf), the slope of the valley (Sl), floor width to valley height (Vf), hypsometric integral (Hi). The index for evaluating relative active tectonic (Iat) basin and sub-basin of the study area were used. Based on the proposed model, recognized three tectonic zones in the study area: (zone with relatively high tectonic activity), this zone is observed only in two sub-basin, 4-B and 9-C, (zone of tectonic activity relative to average) the wide area of the region in this area, it is important that the structures can be noted in the northwest of Dargiaban, Iranshahr fault and fault Saadat-abad, (zone with relatively low tectonic activity) this zone has observations in two sub-basin only 5-C, 1-D, 9A and 8. By comparing and studying index in the range of Taftan volcano and its environment is composed mainly of flysch sediments. The result is that Taftan volcano eruptions of magma has been created in the past and the study area does not have a great impact on tectonic activity, the high indices in this section is affected by magmatic processes up to tectonic, but within the cone of the volcano, control structures such as faults and tectonic activity Saravan and Mirjaveh, Khan Mohammad wells, Saadat-abad and Dargiaban, Iranshahr and etc, and the presence of these faults in the area MORPHOMETRIC PARAMETERS are changed.

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APA: Copy

JAMI, MOHSEN, SALGI, ALI, POORKERMANI, MOHSEN, & MORIDI FARIMANI, ALI ASGHAR. (2017). QUANTITATIVE ANALYSIS OF TECTONIC ACTIVITY IN TAFTAN VOLCANO AND AROUND (SOUTH EAST OF IRAN). JOURNAL OF NATURAL ENVIRONMENT HAZARDS, 5(10), 117-144. SID. https://sid.ir/paper/259114/en

Vancouver: Copy

JAMI MOHSEN, SALGI ALI, POORKERMANI MOHSEN, MORIDI FARIMANI ALI ASGHAR. QUANTITATIVE ANALYSIS OF TECTONIC ACTIVITY IN TAFTAN VOLCANO AND AROUND (SOUTH EAST OF IRAN). JOURNAL OF NATURAL ENVIRONMENT HAZARDS[Internet]. 2017;5(10):117-144. Available from: https://sid.ir/paper/259114/en

IEEE: Copy

MOHSEN JAMI, ALI SALGI, MOHSEN POORKERMANI, and ALI ASGHAR MORIDI FARIMANI, “QUANTITATIVE ANALYSIS OF TECTONIC ACTIVITY IN TAFTAN VOLCANO AND AROUND (SOUTH EAST OF IRAN),” JOURNAL OF NATURAL ENVIRONMENT HAZARDS, vol. 5, no. 10, pp. 117–144, 2017, [Online]. Available: https://sid.ir/paper/259114/en

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