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Relay zones on normal faults accommodate transfer of displacement between adjacent fault segments. We study vertical and horizontal displacement transfer mechanisms across a relay zone adjacent to the Moab Fault at Courthouse Rock (Utah, USA). The relay zone has a reservoir scale (map overlap length ca. 750 m, separation ca. 150 m), and is bounded by two normal fault segments with maximum throw of ca. 12 m. The relay zone is exposed on multiple, sub-parallel cliff faces and intervening rock pavements. We use photogrammetry of these exposures to build a 3D virtual outcrop model of the relay-bounding faults, subordinate faults deforming the relay zone and seven faulted stratigraphic horizons. The relay-bounding faults are right-stepping in map view and contractional in cross-section, defining a relay zone oblique to bedding in 3D. Displacement is transferred both horizontally and vertically across the relay zone. Horizontal transfer of displacement is achieved by a shallow dipping (<1°) relay ramp, whereas vertical transfer is achieved by antithetic faults within the relay ramp. Our analysis demonstrates that multiple mechanisms can work in conjunction to facilitate transfer of displacement across individual relay zones. [Display omitted] • Faults right step in map view but form a contractional step in cross-section, bounding an oblique relay zone in 3D • Displacement is transferred horizontally via a relay ramp and vertically through antithetic faults within the ramp • Multiple mechanisms can work together to facilitate displacement transfer across individual relay zones. [ABSTRACT FROM AUTHOR]

Contractional relay zones between pairs of normal faults are sometimes associated with multiple antithetic faults in a geometry similar to that found in Riedel shear zones. Detailed fault displacement profiles of outcrop examples of this geometry demonstrate that the antithetic faults accommodate the transfer of displacement between the synthetic faults that bound the relay zones. The throw on individual antithetic faults, or R′ shears, is typically constant across relay zones while the throw profile on the synthetic faults, or R shears, is stepped; the steps occurring across branchpoints with abutting R' shears. Transfer of fault displacement occurs by a combination of block rotation and irrotational block translation within the relay zone. As fault throw increases, contractional relay zones are by-passed by the linkage of the synthetic faults, in a manner analogous to the formation of P-shears by the linkage of R shears in classic Riedel shear experiments, but with the original relay zone structure still preserved within the fault zone. With yet further strain bedding may rotate into near-parallelism with the fault surface, with the original geometrical configuration of the relay zone difficult to unravel. • Contractional relay zones on normal faults can be associated with antithetic faults in a Riedel shear zone geometry. • Detailed displacement analysis indicates that antithetic faults convey throw across the contractional relay zones. • With relay breaching, the Riedel shear zone geometry may be deformed by synthetic rotation of bedding and antithetic faults. [ABSTRACT FROM AUTHOR]

The 1:5000 scale Geological Map of the Fontane talc mineralization (FTM) aims to give new information about the origin and geological structure of an important talc mineralization occurring in the axial sector of the Italian Western Alps. The FTM is hosted within a pre-Carboniferous polymetamorphic complex which was deformed and metamorphosed during both Variscan and Alpine orogenesis, and is part of the Dora-Maira continental crust. Field mapping and underground investigations highlight that the talc bodies (i) never crop out but occur at depth along a well-defined lithostratigraphic association between micaschist, marble and gneiss and (ii) were deformed during different Alpine-related deformation phases (i.e. D1, D2and D3syn-metamorphic phases and post-metamorphic extensional faulting). The here defined lithostratigraphic and structural characterization of talc bodies, is an input for further research into the geodynamic context of where talc forms and for new mineral exploration outside the mapped area. [ABSTRACT FROM AUTHOR]

The Taiwan mountain belt is generally thought to develop above a through-going basal thrust confined to within the sedimentary cover of the Eurasian continental margin. Surface geology, magnetotelluric, earthquake hypocenter, and seismic tomography data suggest, however, that crustal levels below this basal thrust are also currently being involved in the deformation. Here, we combine seismic tomography and earthquake hypocenter data to investigate the deformation that is taking place at depth beneath south-central Taiwan. In this paper, we define the basement as any pre-Eocene rifting rocks, and use a P-wave velocity of 5.2 km/s as a reference for the interface between these rocks and their sedimentary cover. We found that beneath the Coastal Plain and the Western Foothills clustering of hypocenters near the basement-cover interface suggests that this interface is acting as a detachment. This detachment is located below the basal thrust proposed from surface geology for this part of the mountain belt. Inherited basement faults appear to determine the geometry of this detachment, and their inversion in the Alishan area result in the development of a basement uplift and a lateral structure in the thrust system above them. However, across the Shuilikeng and the Chaochou faults, earthquake hypocenters define steeply dipping clusters that extend to greater than 20 km depth, above which higher velocity basement rocks are uplifted beneath the Hsuehshan and Central ranges. We interpret these clusters to form a deeply penetrating, east-dipping ramp that joins westward with the detachment at the basement-cover interface. It is not possible to define a basal thrust to the east, beneath the Central Range. [ABSTRACT FROM AUTHOR]

The structure of a caldera may influence its activity, making its understanding crucial for hazard assessment. Here, we analysed high-resolution seismic profiles in the Campi Flegrei (southern Italy) offshore sector. We recognised two main fault systems, including those associated with the formation of the caldera and those affecting the resurgent dome. The former system comprises three broadly concentric fault zones (inner, medial and outer ring fault zones) depicting a nested caldera geometry. Considering the relations between faults and seismic units that represent the marine and volcaniclastic successions filling the caldera, all ring faults were formed during the Campanian Ignimbrite eruption (40 ka) and subsequently reactivated during the Neapolitan Yellow Tuff eruption (15 ka). In this last caldera-forming event, the inner and medial fault zones accommodated most of the collapse and were episodically reactivated during the younger volcano-tectonic activity. The second fault system occurs in the apical zone of the resurgent dome and comprises dominantly high-angle normal faults that are mainly related to the volcano-tectonic collapse that followed the Agnano-Monte Spina Plinian eruption (4.55 ka). Finally, we provide a volcano-tectonic evolutionary model of the last 40 kyr, considering the interplay among ring and dome faults activity, volcaniclastic sedimentation, ground deformation and sea-level changes. • A detailed structural map of the offshore sector of Campi Flegrei caldera is provided. • Two main fault zones have been identified associated with the caldera ring faults and the resurgent dome faults. • The Neapolitan Yellow Tuff eruption reactivated the 2.5 km wide caldera fault zone of the Campanian Ignimbrite eruption. • The dome fault zone accommodated volcano-tectonic collapse during the Agnano-Monte Spina eruption. • Mapped faults controlled caldera deformation, volcanism distribution and hydrothermal fluid uprise in the last 40 kyr. [ABSTRACT FROM AUTHOR]

Faults in volcanic areas can have different origins and can form due to several volcano-tectonic processes. In this work, by means of detailed field observations, we analysed a fault array cutting through a recent pyroclastic succession in the Campi Flegrei caldera of southern Italy to investigate its origin. Geometric and kinematic data indicate that the fault array consists of steeply dipping faults with both normal and reverse senses of movement. Displacement data suggest that these faults with opposed kinematics acted together , in agreement with what was previously described from analogue and numerical experiments for faults formed in response to gravitational collapses in volcanic areas. By integrating these results with considerations of the recent volcano-tectonic evolution of the Campi Flegrei caldera, we propose a model in which the studied fault array developed to accommodate a gravitational collapse triggered by an underground magma migration predating the 1538 CE historical Monte Nuovo eruption. This work is, to our knowledge, the first thorough field description of faults developed to accommodate gravitational collapses in volcanic areas. • Detailed field description and throw analysis of a volcano-tectonic fault array. • Normal and reverse faults of the array acted simultaneously. • The fault array accommodated a gravitational collapse triggered by an underground magma migration. [ABSTRACT FROM AUTHOR]

On 27 March 2013, a 6.2 ML earthquake occurred at 19 km depth in eastern Nantou, central Taiwan. Over a 2 week period it was followed by more than 680 aftershocks that ranged to 5 ML. Most events occurred below the ~10-km-deep detachment fault predicted for this part of the mountain belt, coinciding with other precisely located hypocenters that indicate that much of the crust in this area is seismically active. We combine geological data with a three-dimensional (3-D) P-wave velocity model derived from local tomography and earthquake hypocenters to determine a model for the structure of central Taiwan. Much of the surface geology of the area comprises the uplifted Eocene rocks of the Hsuehshan Basin. The 3-D P-wave velocity model shows a shallowing of higher velocities across the Hsuehshan Basin and hypocenter data indicate that its western bounding fault is clearly defined by an eastward-dipping band of events that extends to >20 km depth. The eastern bounding fault is interpreted to coincide at depth with a cluster of events between 20 and 30 km depth. These data suggest that the preexisting, rift-related extensional faults of the Hsuehshan Basin are currently being reactivated and the basin is being inverted. We present hypocenter data from the Nantou sequence that corroborate this interpretation and show the importance of choosing the correct structural model when assessing seismic risk. [ABSTRACT FROM AUTHOR]

Fault reactivation is a process that has long been described in nature and modelled in the laboratory. Although many plate boundaries worldwide have undergone successive deformation events during one or more Wilson cycles, most often the influence of fault reactivation on mainly the last deformation event can be comprehensively estimated. The northern South China Sea area has undergone, in the last 60 Myr, an entire Wilson cycle associated with the opening and the ongoing closure of the South China Sea oceanic basin. The continental basement that underwent extension during the opening of the South China Sea was associated with at least two, well-defined, systems of faults inherited from the Cretaceous tectonic evolution of the area. Also, the ongoing closure of the northern South China Sea is partial as convergence is highly oblique and collision is very localized and confined to the Taiwan mountain belt, while in most of the Eurasian rifted margin the extensional structures related to the opening of the South China Sea are not yet overprinted. Both these conditions make the northern South China Sea area an ideal one for investigating the significance of fault reactivation throughout the Wilson cycle. In this article, we first review the tectonic history of the northern South China Sea area in the last 60 Myr focusing on how it is reflected on the northern South China Sea rifted margin and the Taiwan mountain belt. We then review the influence that fault reactivation has exerted in these two areas. We found that fault reactivation had a crucial role in accommodating deformation during both the divergence and convergence episodes of the Wilson cycle, and that the degree to which faults are reactivated as well as the style of fault reactivation can be shown to be associated with the angle that inherited faults form with the extension and shortening directions, respectively. Reactivation of faults involving significant remobilisation of basement rocks seems to have been promoted for faults that were forming a high angle with the extension and shortening directions. These results highlight not only the continuous significance that fault reactivation can have during the Wilson cycle undergone at a plate boundary, but also how the first-order, underlying, geometric controls on fault reactivation can display consistency throughout the cycle itself. [ABSTRACT FROM AUTHOR]

Fault zones can often display a complex internal structure associated with antithetic faults, branch and tip points, bed rotations, bed-parallel slip surfaces, and subordinate synthetic faults. We explore how these structural complexities may affect the development of fault-related fractures as displacement accumulates. We analysed in detail an incipient fault zone within well-bedded, shallow-water carbonates of the southern Apennines thrust belt (Italy). The fault zone crops out with quasi-complete exposure at a reservoir scale on an inaccessible sub-vertical cliff face, and fault and fracture mapping were carried out on a 3D virtual outcrop model of the exposure built for this study using photogrammetry. Comparing the structure of the fault zone and the density of 9444 mapped fractures allowed us to unravel their spatial relationships. Our results show that the areas of denser fractures coincide with: (i) rock volumes bounded by antithetic faults developed within the fault zone, (ii) branch points between these antithetic faults and fault zone-bounding fault segments, (iii) fault zone-bounding fault segments associated with significant displacement gradients, and (iv) relay zones between subordinate synthetic faults. These findings may aid locating sub-seismic resolution volumes of dense fracturing and associated enhanced permeability within faulted reservoirs. • Fault zones display complex internal structure. • Fault zone structure affects the density of fault-related fractures. • Variability in fault-related fracture density influences fluid flow in faulted reservoir. • Fault analysis on 3D virtual outcrop model built with photogrammetric techniques. [ABSTRACT FROM AUTHOR]

Normal faults are often complex three-dimensional structures comprising multiple sub-parallel segments separated by intact or breached relay zones. Relay zones are classified according to whether they step in the strike or dip direction and whether the relay zone-bounding fault segments are unconnected in 3D or bifurcate from a single surface. Complex fault surface geometry is described in terms of the relative numbers of different types of relay zones to allow comparison of fault geometry between different faults and different geological settings. A large database of fault surfaces compiled primarily from mapping 3D seismic reflection surveys and classified according to this scheme, reveals the diversity of 3D fault geometry. Analysis demonstrates that mapped fault geometries depend on geological controls, primarily the heterogeneity of the faulted sequence and the presence of a pre-existing structure, as well as on resolution limits and biases in fault mapping from seismic data. Where a significant number of relay zones are mapped on a single fault, a wide variety of relay zone geometries occurs, demonstrating that individual faults can comprise segments that are both bifurcating and unconnected in three dimensions. • A large database of 3D fault surface geometry from different geologic settings. • Comparison of fault surface geometry based on segmentation characteristics. • Faults typically comprise both bifurcating and unconnected segments. • Fault geometry is controlled by the heterogeneity of the faulted sequence and pre-existing structure. [ABSTRACT FROM AUTHOR]

The Mountain Front Flexure is a major structure of the Zagros orogenic system, and is underlain by the deeply rooted and seismically active Mountain Front Fault system. These coupled structural features divide the belt from its foreland and their trace is sinuous, forming salients and recesses. The origin and tectonic significance of the Mountain Front Fault system and its sinuosity are still unclear, with most of hypotheses pointing to a strong structural control exerted by geological inheritances. In this work we combine interpretation of seismic reflection profiles, earthquake data, geomorphic analysis, and geological observations, to build a balanced cross section across the Mountain Front Flexure in the Lurestan region. Our data are suggestive of a hybrid tectonic style for the Lurestan region, characterised by a major and newly developed crustal ramp in the frontal portion of the belt (i.e the Mountain Front Fault) and by the reactivation of steeply dipping pre-existing basin-bounding faults, along with a minor amount of shortening, in the inner area. Specifically, the integration of our results with previous knowledge indicates that the Mountain Front Fault system developed ahead of an array of inverted Jurassic extensional faults, in a structural fashion which resembles that of a crustal-scale footwall shortcut. Within this structural context, the sinusoidal shape of the Mountain Front Flexure in the Lurestan area arises from the re-use of the original segmentation of the inverted Jurassic rift system. Image 1 • Balanced cross section across the Lurestan arc indicate inversion tectonics. • The Mountain Front Flexure develops ahead of an array of inverted faults. • Sinuosity of the Mountain Front Flexure relates with Jurassic rift inheritances. [ABSTRACT FROM AUTHOR]

Individual normal faults are rarely single planar surfaces and often comprise arrays of fault segments arising from the earliest stages of fault propagation. Current models for the geometry and formation of relay zones between adjacent fault segments have been informed mainly by 2D analysis from either maps or cross-sections observed in outcrop and, to a lesser extent, by the analysis of relay zones from 3D seismic reflection data. Using high quality 3D seismic reflection datasets from a selection of sedimentary basins, we investigate fundamental characteristics of segmentation from the analysis of 67 normal faults with modest displacements (

This article presents a personal narrative by the author on his disillusionment regarding his work as a postdoctoral fellow, citing burnout, competition, and pressure.

The 3‐D structure of continental metamorphic core complexes (MCCs) and their coevolution along with the associated extensional detachments are still not well understood. In this study, analysis of a newly acquired high‐resolution 3‐D seismic reflection volume reveals for the first time a well‐imaged MCC in the proximal northern South China Sea (SCS) rifted margin, the Kaiping MCC (KP MCC). These data provide a 3‐D view of the KP MCC and the associated KP detachment fault. The KP MCC is characterized by ascend of ductile midcrustal materials, and it is partially exhumed in the KP9 High. The KP detachment fault displays a domed low‐angle geometry, and is characterized by pronounced NS‐plunging corrugations, among which two megacorrugations of tens of kilometers are revealed. Evidence show that the KP MCC developed according to the classical rolling‐hinge model. A group of secondary normal faults and fractures, which are parallel to the axis of the KP MCC and offset the KP detachment surface at the crest of the MCC, developed in response to inelastic bending during progressive warping of the footwall. The migration of the domal seismic reflection layers provides a visual evidence for the kinematic process of the rolling‐hinge activity, during which the brittle‐ductile transition and the rolling hinge gradually migrate as the detachment fault slips. The origin of the KP MCC in the northern SCS margin is suggested to have been favored by the existence of a pre‐existing midcrustal ductile layer and basement structures within the upper brittle crust. Plain Language Summary: A metamorphic core complex (MCC) is an exposure of deep crust associated with extensional processes. Current understanding on MCCs is mainly derived from outcrop and geomorphic studies that only allow their exhumed part to be observed. A newly acquired 3‐D seismic reflection volume reveals a well‐imaged MCC, the Kaiping MCC (KP MCC), in the proximal northern South China Sea (SCS) rifted margin, permitting, for the first time, a detailed 3‐D examination of the MCC structure and its associated detachment fault. In this study, we present the 3‐D structure of the KP MCC, the geometry and kinematics of the associated KP detachment fault, and then we discuss the development and origin of the KP MCC. We propose that the KP MCC developed according to the rolling‐hinge model, with our data providing a visual evidence for the kinematic processes during which the brittle‐ductile transition and the rolling hinge gradually migrate as the detachment fault slips. We suggest that the origin of the KP MCC is favored by the existence of a pre‐existing midcrustal ductile layer and basement structures within the upper crust. Our study not only have implication for the SCS rifting but also advance understanding on the development and origin of MCCs. Key Points: A first imaged metamorphic core complex (MCC) in the proximal northern South China Sea rifted margin and its 3‐D structure is describedVisual evidence for the gradual migration of the brittle‐ductile transition and rolling hinge during the rolling‐hinge evolution of a MCCThe origin of the MCC was favored by a pre‐existing midcrustal ductile layer and basement structures within the upper crust [ABSTRACT FROM AUTHOR]

In accretionary convergent margins, the subduction interface is formed by a lower plate décollement above which sediments are scraped off and incorporated into the accretionary wedge. During subduction, the basal décollement is typically located within or at the base of the sedimentary pile. However, the transition to collision implies the accretion of the lower plate continental crust and deformation of its inherited rifted margin architecture. During this stage, the basal décollement may remain confined to shallow structural levels as during subduction or re-localize into the lower plate middle-lower crust. Modes and timing of such re-localization are still poorly understood. We present cases from the Zagros, Apennines, Oman, and Taiwan belts, all of which involve a former rifted margin and point to a marked influence of inherited rift-related structures on the décollement re-localization. A deep décollement level occurs in the outer sectors of all of these belts, i.e., in the zone involving the proximal domain of pre-orogenic rift systems. Older--and shallower--décollement levels are preserved in the upper and inner zones of the tectonic pile, which include the base of the sedimentary cover of the distal portions of the former rifted margins. We propose that thinning of the ductile middle crust in the necking domains during rifting, and its complete removal in the hyperextended domains, hampered the development of deep-seated décollements during the inception of shortening. Progressive orogenic involvement of the proximal rift domains, where the ductile middle crust was preserved upon rifting, favors its reactivation as a décollement in the frontal portion of the thrust system. Such décollement eventually links to the main subduction interface, favoring underplating and the upward motion of internal metamorphic units, leading to their final emplacement onto the previously developed tectonic stack. [ABSTRACT FROM AUTHOR]

Abstract The Late Cretaceous is a significant geologic period in the South China Sea area, as it marks the tectonic transition from the early Paleo-Pacific Plate subduction to the subsequent Cenozoic rifting related to the opening of the SCS. However, the Late Cretaceous tectonic evolution of the South China Sea area is yet to be clearly defined, and it is at present largely debated in the literature. In this paper, mainly on the basis of ~240,000 km2 newly acquired 3D seismic reflection data, 94 industrial wells and existing U Pb ages of basement granitoids, we carried out an integrated interpretation, mapping and analysis of the pre-Cenozoic (> 66 Ma) structures within the basement of the Cenozoic rift basin in the northern South China Sea area, that can be crucial for a broad understanding of the Late Cretaceous tectonic evolution of this region. Results of this analysis suggest that three Late Cretaceous fault systems can be identified in the northern South China Sea margin: 1) the WNW-striking thrust system, 2) ENE-striking extensional fault system, and 3) ENE-striking thrust system. These three fault systems are considered to have developed in the Late Cretaceous since they are superimposed on the well dated Late Jurassic to Early Cretaceous (161.6–101.7 Ma) arc-related granitoids that define most of the basement of the Cenozoic rift basin within the study area. This new structural evidence, combined with a review of previous studies, led us to propose a renewed multi-phase geodynamic evolutionary model of the South China Sea area during the Late Cretaceous. The first tectonic event that can be recognized generated the WNW-striking thrust system and is, in this paper, interpreted to have formed as a result of a sinistral transpressional event that took place in the South China Sea area and adjacent areas around 100 Ma at the Early-Late Cretaceous boundary. This transpressional event was likely related to intense oblique convergence between the Paleo-Pacific Ocean Plate and the Eurasia Plate. The second tectonic phase that was identified in this paper (~100 Ma to ~72 Ma) is defined by an extensional event that generated the largely ENE-striking extensional fault systems and associated basins, which is interpreted to be related to the back-arc extension that took place in this period in response to the slab roll back and high-angle subduction of the Paleo-Pacific Plate. This extensional phase eventually led to the opening of the Proto-South China Sea on the SE margin of the proto-South China Block, and it should be distinguished from the Cenozoic rifting phases that are related to the opening of the South China Sea. The third and last tectonic phase that was recognized in this paper is a compressional event that took place in the late stage of the Late Cretaceous (~72 Ma to ~66 Ma) and was responsible for the development of the ENE-striking thrust system. We suggest that this post-subduction (post-Yanshanian) compressional event can be interpreted to have developed in response to process of ridge push related to the sea floor spreading of the Proto-South China Sea. Highlights • Two Late Cretaceous (K 2) thrust systems and one extensional fault system are identified in the northern SCS area • A sinistral transpressional event at the Early-Late Cretaceous boundary in response to a change in plate configuration • An episode of regional extension related to the back-arc extension in the early K 2 in the SCS area • A previously unrecognized compressional event caused by ridge push process of the Proto-SCS opening in the late K 2 • A renewed multi-phase geodynamic evolutionary model of the SCS area during the Late Cretaceous [ABSTRACT FROM AUTHOR]

The basement structure of the Cenozoic Enping Sag, within the Pearl River Mouth Basin on the northern margin of South China Sea, is revealed by borehole-constrained high-quality 3D seismic reflection data. Such data suggest that the Enping Sag is bounded in the north by a low-angle normal fault. We interpret this low-angle normal fault to have developed as the result of the reactivation of a pre-existing thrust fault part of a pre-Cenozoic thrust system. This is demonstrated by the selective reactivation of the pre-existing thrust and by diffuse contractional deformation recognized from the accurate analysis of basement reflections. Another significant result of this study is the finding of some residual rift basins within the basement of the Enping Sag. Both the thrust system and the residual basins are interpreted to have developed after the emplacement of continental margin arc-related granitoids (J 3 –K 1 ) that define the basement within the study area. Furthermore, seismic sections show that the pre-existing residual rift basins are offset by the main thrust fault and they are both truncated by the Tg unconformity. These structural relationships, interpreted in the frame of previous studies, help us to reconstruct a six-event structural evolution model for the Enping Sag from the late Mesozoic to the early Cenozoic. In particular, we interpret the residual rift basins to have formed as the result of back-arc extension due to the slab roll-back of the Paleo-Pacific Plate subduction in the early K 2. The thrust system has recorded a compressional event in the late K 2 that followed the back-arc extension in the SCS area. The mechanism of this compressional event is still to be clarified, and might be related to continuous subduction of the Paleo-Pacific Plate or to the continent-continent collision between a micro-continental block and the South China margin. [ABSTRACT FROM AUTHOR]

Defining the origin of ground deformation, which can be a very challenging task, may be approached through several investigative techniques. Ground deformation can originate in response to both natural (e.g., tectonics) and anthropic (e.g., groundwater pumping) contributions. These may either act simultaneously or be somewhat correlated in space and time. For example, the location of structurally controlled basins may be the locus of enhanced human-induced subsidence. In this paper, we investigate the natural and anthropic contributions to ground deformation in the urbanized area of the inner Sarno plain, in the Southern Apennines. We used a multidisciplinary approach based on the collection and analysis of a combination of geomorphological, stratigraphical, structural, hydrogeological, GPS, and DInSAR datasets. Geomorphological, stratigraphical, and structural data suggested the occurrence of a graben-like depocenter, the Sarno basin, bounded by faults with evidence of activity in the last 39 ka. Geodetic data indicated that the Sarno basin also experienced ground deformation (mostly subsidence) in the last 30 years, with a possible anthropogenic contribution due to groundwater pumping. Hydrogeological data suggested that a significant portion of the subsidence detected by geodetic data can be ascribed to groundwater pumping from the alluvial plain aquifer, rather than to a re-activation of faults in the last 30 years. Our interpretation suggested that a positive feedback exists between fault activity and the location of area affected by human-induced subsidence. In fact, fault activity caused the accumulation of poorly consolidated deposits within the Sarno basin, which enhanced groundwater-induced subsidence. The multidisciplinary approach used here was proven to be successful within the study area and could therefore be an effective tool for investigating ground deformation in other urbanized areas worldwide. [ABSTRACT FROM AUTHOR]

Extensive opencast lignite mining in the Ptolemais Basin, NW Greece has exposed a plethora of outcrops within a normal fault system offsetting a sequence of interbedded lignites and marls of Pliocene age. The entire length of a 630 m long fault over a vertical interval of 80 m has been mapped in detail from 48 mine faces. The mapped fault comprises 5 fault segments large enough to be mapped in 3D, smaller fault segments exposed on individual mine faces and associated continuous deformation in the form of bed rotations and normal drag. These fault components combined to provide a regular aggregate throw distribution over the mapped fault. The boundaries between adjacent fault segments have a variety of geometries and they may be fully unconnected or they may link along strike or down dip within the fault zone. The fault geometry and throw distribution is analysed using two approaches, a discrete mapping of the large fault segments and a continuous approach based on measures of fault thickness and throw partitioning at individual outcrops. This combination of approaches demonstrates that fault thickness and the proportion of fault throw on the individual fault segments observed on any cross-section through the fault are related almost entirely to fault segmentation in 3D. • An exceptionally well exposed normal fault has been mapped in detail using complementary discrete and continuous approaches. • The fault comprises bifurcated fault surfaces, unconnected surfaces in 3D but geometrically coherent, and partially breached relays. • The 3D fault segmentation and geometries at mapped segment boundaries occur over a wide range of scales. • The irregular fault thickness distribution and the partitioning of throw are controlled by the large-scale 3D fault segmentation. • The distribution of the aggregate throw indicates a geometrically and kinematically coherent array of fault segments. [ABSTRACT FROM AUTHOR]