Open Access
Newly Discovered Mud Volcanoes, Mechanism, Geomorphological and Geochemical Characteristics in the Coastal Belt of Makran, Iran
TLDR
In this paper, Iran's coastal, including topography and geology maps, IRS satellite data and aerial photos, remote sensing verifications were implemented, then, mud volcanoes determination was completed by field work studies and checking.Abstract:
Mud volcanism is a global phenomenon usually associated with compressional tectonics that favor extrusion of fluid- and clay mineral-rich sediment both on land and offshore. Iran's coastal, bordering the western Makran Coast, has more than 50prominent onshore MVs. In this research, after data collection, including topography and geology maps, IRS satellite data and aerial photos, remote sensing verifications were implemented. Then, mud volcanoes determination was completed by field work studies and checking. Their geomorphology characteristic such as area and height were measured. One sediment and one water samples were taken from each mud volcano in the field work, then analyses of major, minor and trace elements were carried out through ICP -OES. About 20 small or big mud volcanoes were determined in Hormozgan province that they have not been introduced before. In the meantime, hydro geochemistry studies or determination of the percentage of available elements in water for all mud volcanoes were implemented. Since this geomorphological phenomenon indicates tectonic activity of a region, hence there is a possibility of mild earthquake and faulting occurrence. After determine correlation analysis cluster and factor analysis determine between different factors from scoter plot map characterized that source of elements Al, Fe, Ni, V, Sc, Ti, Cr, Zn, Cu, Mn, Na, K, Li, Be is geogenic and source of elements Ca,Mn and S is biogenic.read more
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Journal Article
Mud volcanism on the Mediterranean Ridge: initial results of Ocean Drilling Program Leg 160
TL;DR: In this article, during Ocean Drilling Program Leg 160 (April-May, 1995), two mud volcanoes within the Mediterranean Ridge accretionary complex were studied, one of which is at least 1.75 million years old and the other is currently active.
References
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Journal ArticleDOI
Current plate motions
TL;DR: A global plate motion model, named NUVEL-1, which describes current plate motions between 12 rigid plates is described, with special attention given to the method, data, and assumptions used as discussed by the authors.
Current plate motions
TL;DR: In this paper, a new global model (NUVEL-1) was proposed to describe the geologically current motion between 12 assumed-rigid plates by inverting plate motion data.
Journal ArticleDOI
Significance of mud volcanism
TL;DR: The authors summarizes the main thrusts in mud volcano research as well as the various regions in which mud volcanism has been described, including the collision zones between Africa and Eurasia, where fluid flux through mud extrusion exceeds the compaction-driven pore fluid expulsion of the accretionary wedge.
Book
Seabed Fluid Flow: The Impact on Geology, Biology and the Marine Environment
Alan Judd,Martin Hovland +1 more
TL;DR: In this article, the authors introduce seabed fluid flow around the world and discuss the nature and origins of flowing fluids, and the role of seabing fluid flow in the hydrosphere and atmosphere.
Journal ArticleDOI
Worldwide distribution of submarine mud volcanoes and associated gas hydrates
TL;DR: The list of known and inferred deep-water mud volcanoes is presented in this article, where a preliminary global estimate of methane accumulated in gas hydrates associated with mud volcano is about 1010-1012 m3 at standard temperature and pressure.