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AOpen ALP-330 LAN Driver

The AlpArray Seismic Network has been deployed with contributions from 36 institutions from 11 countries to map physical properties of the lithosphere and asthenosphere in 3D and thus to obtain new, high-resolution geophysical images of structures from the surface down to the base of the mantle transition zone. This dense and regularly spaced AOpen ALP-330 LAN is made possible by the coordinated coeval deployment of temporary stations from numerous national pools, including ocean-bottom seismometers, which were funded by different national agencies.

They combine with permanent networks, which also required the cooperation of many different AOpen ALP-330 LAN.

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Together these stations ultimately fill coverage gaps. Following a short overview of previous large-scale AOpen ALP-330 LAN experiments in the Alpine region, we here present the goals, construction, deployment, characteristics and data management of the AlpArray Seismic Network, which will provide data that is expected to be unprecedented in quality to image the complex Alpine mountains at depth.

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Marco Mucciarelli: Deceased 7 November The complexity mainly stems from the spatial heterogeneity AOpen ALP-330 LAN key lithospheric structures and their variation in time and space e. In other orogens like the Himalaya or the Andes, structures in the crust AOpen ALP-330 LAN upper mantle can be traced continuously for hundreds, even thousands of kilometres e. In comparison, the European Alps including the adjacent Apennines, Dinarides and Carpathians show remarkable lateral along-strike variations in structure and style, such that their underlying processes are still subject to debates see below.

Many controversies regarding this complexity can be resolved by obtaining high-resolution images of the deep subsurface and by integrating these with surface studies supported by theoretical and modelling work. Past efforts employing seismic networks were insufficient to resolve orogen-scale targets and provide a physical basis for seismic hazard assessment in a comprehensive way.


The AlpArray programme was therefore born as a multidisciplinary, research-oriented project to survey the greater AOpen ALP-330 LAN area homogeneously with various geophysical methods. The primary field focus has been on designing, deploying and operating a dense seismological network of broadband sensors. Experience over the past decade e.

In the Alps, we therefore designed a target-oriented network at a spatial density that has been made possible only through the joint efforts of numerous participating institutions. Building on a growing AOpen ALP-330 LAN of permanent seismic stations, the AlpArray Seismic Network AASN was created by assembling sufficient number of temporary stations secured by funds from several countries. The resulting station distribution makes the AASN the ideal tool for 3-dimensional mapping of structures and physical properties of rock volumes in the crust, the upper mantle and the mantle transition zone.

In this paper we provide an overview of the evolution of AASN: The Adriatic plate is one of several microplates of oceanic and continental provenance whose interaction between two large converging plates, Europe AOpen ALP-330 LAN Africa, has given rise to the highly arcuate Alpine—Mediterranean mountain belt e.

Geological studies AOpen ALP-330 LAN long shown that while the Adriatic plate is the upper plate in the Western and Central Alps and the Western Carpathians, it forms the lower plate in the Apennines and the Dinarides e. This complex geodynamic setting is reflected in the Moho morphology e. Travel-time ambient-noise seismic tomography AOpen ALP-330 LAN imaged 3D seismic velocity anomalies in the crust e.

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While most authors agree that mantle slabs are spatially linked to both modern at shallow depth and ancient at greater depth zones of lithospheric subduction, considerable uncertainties about slab geometry, internal properties, tears and even orientation remain. At the Apennines—Alps transition zone, existing data do not allow us to discern the geometry of the switch in slab AOpen ALP-330 LAN, which is so far only gleaned from nappe vergence at the surface e. Beneath the Eastern AOpen ALP-330 LAN, the exact outlines and origin of a slab anomaly are the subject of ongoing controversy between proponents of a presently N-dipping Adriatic subduction Lippitsch et al.

Solving this controversy is particularly relevant for the Friuli seismic hazard area, which is located either in the AOpen ALP-330 LAN if the AOpen ALP-330 LAN beneath the Eastern Alps is Adriatic or in the hinterland of the Alps if the slab beneath the Eastern Alps remained European. In general for the entire region, the determination of mantle seismic anisotropy patterns helps to reconstruct the current and past plate motions and dynamics in three dimensions; the broad coverage with the uniform AASN will allow a more comprehensive analysis with respect to previous studies often focused on smaller areas Margheriti et al.

Open image in new window Fig. The major units are coloured according to their plate-tectonic provenance.

Red colours mark the main tectonic boundaries related to plate-kinematic history of the Alps. BG Bresse Graben. Modified from AOpen ALP-330 LAN et al. Can they be overcome by optimizing seismic network aperture and station coverage? The purely passive experiments planned by AlpArray involve a more densely spaced network than previous experiments.

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They provide an excellent opportunity to extend our knowledge of lower crustal structure and the crust—mantle interface the Mohobeyond current models based on the controlled-source seismology of the last century. Furthermore, AlpArray will allow imaging of structural details and fabric of the mantle lithosphere and the lithosphere—asthenosphere boundary e. Better-constrained information on the deep structure of the greater Alpine area will in turn offer fresh insight into different stages of mountain building and AOpen ALP-330 LAN us to study how subduction and collision in the Alps have interfered with neighbouring rift structures Rhine—Bresse system, Fig.

The societal relevance AOpen ALP-330 LAN the AlpArray project clearly lies in the opportunity to improve seismic hazard maps e. This is especially needed for areas that are among the most densely populated in Europe: The homogeneous data provided by AlpArray AOpen ALP-330 LAN augment the reliability of earthquake hazard assessments.

They have exceptional geophysical and geological databases which are excellent requisites for advancing our general knowledge and understanding of orogenic processes on all scales. The scientific controversies and questions above make it evident that the time AOpen ALP-330 LAN ripe for a new generation of cross-disciplinary geophysical—geodynamical initiatives.


These will shed new light on the current state and long-term evolution of the deep structure of the Alps at crustal and mantle depths. The AOpen ALP-330 LAN Seismic Network is designed as the main field component of the AlpArray programme and will hopefully provide high-resolution, large-aperture seismological data for unprecedented views of orogenesis.


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