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Ôø Å Òù× Ö Ôø ÔØ ÅÒÙ×Ö ÔØ Hydromagmatic eruption during the buildup of a Triassic carbonate platform (Oman Exotics): Eruptive style and associated deformations Christophe Basile, Franc¸ois Chauvet PII: S0377-0273(09)00145-0 DOI: doi: 10.1016/j.jvolgeores.2009.03.009 Reference: VOLGEO 4286 To appear in: Journal of Volcanology and Geothermal Research Received date: 20 October 2008 Accepted date: 11 March 2009 Please cite this article as: Basile, Christophe, Chauvet, Fran¸cois, Hydromagmatic erup- tion during the buildup of a Triassic carbonate platform (Oman Exotics): Eruptive style and associated deformations, Journal of Volcanology and Geothermal Research (2009), doi: 10.1016/j.jvolgeores.2009.03.009 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. In press, Journal of Volcanology and Geothermal Research Hydromagmatic eruption during the buildup of a Triassic carbonate platform (Oman Exotics): eruptive style and associated deformations Christophe Basile (corresponding author), François Chauvet (1) Laboratoire de Géodynamique des Chaînes Alpines, CNRS UMR 5025, Observatoire des Sciences de l’Univers de Grenoble, Université Joseph Fourier Maison des Géosciences, 1381 rue de la Piscine 38400 St Martin d’Hères, France tel. 334 765 140 69 fax 334 765 140 58 email [email protected] ; [email protected] (1) present adress: Laboratoire de Planétologie et Géodynamique de Nantes, CNRS UMR 6112, Université des Sciences de Nantes, 2 rue de la Houssinière, BP92208, 44322 Nantes Cedex 3, France Abstract Oman Exotics represent remnants of a Triassic carbonate platform, also named Misfah Formation. Several basaltic intrusions or lava flows were coeval with the carbonate platform build-up. We present field observations related to one of these volcanic events, including associated deformation of the host rocks and interaction of volcanism with the sedimentation. These observations allow us to reconstruct the structure of the volcanic conduit and vent and the successive stages of the evolution of the eruption. The initial ascent of magma probably occurred along on a normal fault related to gravity-driven sliding towards the platform edge. Magma was first emplaced in a saucer-shaped sill a few tens of meters below the sea-floor. This intrusion provided a decollement layer, that may have sped up the gravity-driven sliding, opening fractures that brought sea-water into contact with the magma, hence triggering a hydromagmatic eruption. Eruption was followed by the collapse of the host limestones that formed a megabreccia infilling the eruptive vent and prohibiting further contact between sea water and magma. Most of the magma was emplaced at depth in two superposed small magmatic bodies (300 x 100 m and 200 x 50 m in sections, respectively) that replaced the host sediments and uplifted the overlying vent. Despite the shallow submarine setting, this eruption produced a vent quite similar to subaerial maars developped in soft substrate. This emphasizes that the rheology of the substrate may be more important than the amount of water to control magma-water interaction in hydromagmatic eruptions. In an active carbonate platform like Misfah Formation during Triassic times, the early diagenesis of lime mud determined the mechanical comportment of the sediment at the time of eruption, and especially the way it could be mixed with the magma and/or slide into the vent. Keywords Phreatomagmatic eruption; sill; magma stock; megabreccia; carbonate platform ; diatreme _____________________________________________________________________________________ 1. Introduction with water (Sheridan and Wohlez, - shallow-marine Surstey-type Since the birth of Surtsey 1983) or water-rich sediments (White, eruptions (e.g. Kokelaar, 1983), where (Thorarinsson, 1967; Kokelaar, 1983) 1996), and with the local conditions magma enters within a large volume of and Capelinhos (Machado et al., 1962; that bring magma and water into surface water. The interaction of Cole et al., 2001) volcanic islands, the contact. Many examples of magma with water in excess produces interaction of magma and external hydromagmatic eruptions have been numerous explosions that build tuff water appeared as one of the most described all over the world, and over cones and/or rings by fallout and important factors influencing the various types of substratum. The two pyroclastic surges (Cole et al., 2001; volcanic eruption processes (Sheridan main types are: Solgevik et al., 2007). and Wohletz, 1983; Zimanowski et al., - subaerial maars (e.g. Lorenz, Carbonate platforms represent a 1991). This interaction results from an 1974), where magma encounters large proportion of shallow-marine efficient heat transfer from the magma ground or underground water. The environments, but we found only a few to the water, generating large amounts evolution of this type of volcano published observations of volcanic of steam. When lava and water come depends on the rheology of the eruptions during carbonate platform together in an underground closed substratum (soft- and hard-substrate build-up. In most cases, carbonate space, the increasing volume of steam maars: Lorenz, 2003; Sohn and Park, platforms developed above or on the may induce overpressure, triggering an 2005; Martin and Nemeth, 2005; Auer side of inactive volcanoes, either in explosive reaction and hydromagmatic et al., 2007), and on the way water and intraplate settings (e.g. Hess, 1946; eruption. The morphology, structure magma circulate to produce a series of Matthews et al., 1974), or in and lithology of the volcanic edifices explosions within the diatreme (Lorenz subduction-related volcanic arcs (e.g. built by hydromagmatic eruptions vary and Kurzlaukis, 2007). Fulthorpe and Schlanger, 1989; Soja, with the ratio of magma interacting 1996). When volcanism and carbonate 1 In press, Journal of Volcanology and Geothermal Research a continental slope (Sumeini Formation: Glennie et al., 1974), and basinal environments (Hawasina Formations: Glennie et al., 1974; Béchennec, 1988). Sumeini and Hawasina formations were thrusted on the arabian platform during the upper Cretaceous obduction of the Sumail ophiolites (Béchennec et al., 1988) (Fig. 1). It is noteworthy that the paleopositions of the sedimentary units on the continental margin were mainly derived from their positions in the tectonic pile, assuming an outward thrust sequence (Glennie et al., 1973, 1974; Béchennec, 1988; Robertson and Searle, 1990). There is an ongoing debate on the nature of the basement below the Hawasina basin, supposed to be either oceanic (Glennie et al., 1973, 1974; Stampfli et al., 1991; Pillevuit et al., 1997), continental (Béchennec, 1988; Béchennec et al., 1990, 1991) or intermediate (Graham, 1980; Searle Figure 1: Location of the studied area (Jabal Misfah, boxed) in a simplified and Graham, 1982). As a consequence, geological map of central and eastern Oman Mountains (modified after the Permian (e.g. Pillevuit et al., 1997) Béchennec et al., 1990). Inset: simplified geological map of northern Oman, or Triassic (e.g. Béchennec, 1988) age modified after Glennie et al., 1974. for the onset of the oceanic accretion is also a matter of debate. During Triassic times, a carbonate platform sedimentation are coeval, they However, this study based on drilling platform developed within the are mainly restricted to cores does not provide information at Hawasina basin. Because they are interstratification of sediments and lava the vent scale nor for the successive mainly found in tectonic slices, flows or volcanic fallouts (e.g. Buigues stages of the eruption. remnants of this platform were named et al., 1992; Soja, 1996; Beltramo, In this paper, we describe the Oman Exotics by Glennie et al. (1974). 2003). interaction of a volcanic eruption with They were referred to the Kwar Group We found only a few examples of the formation of a Triassic carbonate by Béchennec (1988). In the Hawasina volcanism contemporaneous with a platform in Oman. Since a full section nappes, the Kwar Group crops out growing carbonate platform, such as of this volcanic edifice outcrops, it mainly south of the western the Triassic dikes and lavas emplaced provides outstanding observations of termination of Jabal Akhdar anticline in the Dolomites (Southern Alps : the geometry of the vent, of the in several mountains dominated by Blendinger, 1985), or an Albian successive stages of the eruption, and high carbonate cliffs: Jabal Misht, basaltic intrusion and associated allows one for the first time to evaluate Jabal Misfah, Jabal Kwar, Jabal Ghul volcaniclastic sediments in Spain the respective evolutions of the feeding (Fig. 1). This Group has been divided (Fernández-Mendiola and García- system, water-magma contact zone and by Béchennec (1988) into four Mondéjar, 2003). Actually, the best subsea volcanic edifice, emphasizing Formations, later-on subdivided into described example of shallow-marine associated small- and large-scale six Formations by Pillevuit (1993). eruption through a growing carbonate deformations. Stratigraphy has been defined on the platform is the MIT guyot in the northern and eastern
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