Mud volcano growth by radial expansion: Examples from onshore Azerbaijan. (February 2020)

• Record Type: Journal Article
• Authors: Odonne, Francis; Imbert, Patrice; Dupuis, Matthieu; Aliyev, Adil A.; Abbasov, Orhan R.; Baloglanov, Elnur E.; Vendeville, Bruno C.; Gabalda, Germinal; Remy, Dominique; Bichaud, Victoria; Juste, Rémy; Pain, Maëlys; Blouin, Arthur; Dofal, Anthony; Gertauda, Mathieu
• Is Part Of: Marine and petroleum geology. Volume 112(2020)
• Publication Date: 2020-02
• Subjects: Flat-topped mud-volcanoes -- Azerbaijan -- Growth of flat mud volcanoes -- Resistivity-gravity data -- Low-density mud at depth -- Mudflows stacking -- Soft mud; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2019.104051
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: We investigated the mode of growth of flat-topped mud volcanoes, through the study of three active edifices onshore Azerbaijan: they are the Bozdag-Guzdek, the Ayazakhtarma and the Akhtarma-Pashaly mud volcanoes. The three edifices are up to 80 m high and 3 km wide, and have eruptions with recurrent times from a few months to a few years. Surface changes during and between eruptions were documented by a combination of mapping from satellite pictures, repeated direct observation over five years and structural analysis. In addition, resistivity profiles and microgravity measurements were used to decipher their subsurface geometries. We interpret the flat-topped character of the mud volcanoes as the result of rapid "isostatic" readjustment of a brittle surface crust, < 1 m to tens of meters thick, overlying a ductile layer. The surface structure typically shows a concentric transition from an extensional regime in the vicinity of the emission center, to strike slip movements in a median ring, to a compressional regime with thrusts, and pop-up blocks or folds in the outer part of the plateau. Both the flat surface of these mud volcanoes and observed radial displacements of the surface, combined with the very low Bouguer anomaly of the Ayazakhtarma mud volcano, give arguments to propose that km-diameter, flat-topped mud volcanoes likely reflect the presence at a shallow depth (a few tens of meters?) of a large volume of soft mud. Rapid compaction at the surface forms a crust that moves away from a central feeding area, thereby transferring mud added at the center into lateral spreading, building a Coulomb prism all around the mud volcano and strongly limiting vertical buildup. Highlights: We propose a new model of growth for flat-topped mud volcanoes fed from the center. Flat-topped MVs grow by radial expansion, making a concentric structural pattern. Fractures evolve from extensional in center to compressional at periphery. Gravity inversion shows a ca 300 m thick low-density lens below the surface. Soft mud in the lens limits vertical growth and flattens the MV by isostasy.