Distinguishing tectonically-and gravity-driven synsedimentary deformation structures along the Apulian platform margin (Gargano Promontory, southern Italy)

Acknowledgements This work has been supported by Reservoir Characterisation Project (www.rechproject.com) and FAR Project 2014 "Characterisation and modelling of natural reservoirs of geofluids in fractured carbonate rocks", funded by the University of Camerino, coordinator Emanuele Tondi.

Paleoambiente e diagênese da formação Itaituba, carbonífero da bacia do Amazonas, com base em testemunho de sondagem, região de Uruará, Pará

A Formação Itaituba de idade carbonífera representa a sedimentação carbonática de depósitos transgressivos do Grupo Tapajós da Bacia do Amazonas. A sucessão Itaituba é interpretada como depósitos de planície de maré mista, constituídos de calcários fossilíferos, dolomitos finos, arenitos finos a grossos e subordinadamente siltitos avermelhados, evaporitos e folhelhos negros. A análise de fácies e microfácies do testemunho de sondagem da região de Uruará, Estado do Pará, permitiu individualizar dezenove fácies agrupadas em cinco associações: planície de maré (AF1), canal de maré (AF2), laguna (AF3), barra bioclástica (AF4) e plataforma externa (AF5). AF1 é composta por arenito fino com rip-up clasts e gretas de contração, marga com grãos de quartzo e feldspato, dolomudstone laminado com grãos terrígenos e dolomito fino silicificado, com intercalação de argilito com grãos de quartzo disseminados, dolomitizado e localmente com sílica microcristalina. AF2 consiste em arenito médio a grosso com estratificação cruzada acanalada, recoberta por filmes pelíticos nos foresets, arenito muito fino a fino com acamamento wavy, siltito laminado com falhas sinsedimentares e acamamento convoluto. AF3 é constituída de siltito vermelho maciço, mudstone com fósseis, floatstone com braquiópodes e pirita disseminada e mudstone maciço com frequentes grãos de quartzo. AF4 e AF5 exibem abundantes bioclastos representados por espinhos e fragmentos de equinodermas, conchas, fragmentos e espinhos de braquiópodes, ostracodes, foraminíferos, algas vermelhas e conchas de bivalves. AF4 é formada por grainstone oolítico fossilífero e grainstone com terrígenos principalmente grãos de quartzo monocristalino e AF5 se compõe de wackestone fossilífero, wackestone com terrígenos e mudstone maciço com grãos de quartzo monocristalino. Subarcósios (AF1), arcósios (AF2) e arcósios líticos (AF2) são os tipos de arenitos da sucessão Itaituba e apresentam como principais constituintes grãos de quartzo monocristalino e policristalino, K-feldspato, plagioclásio, pirita, muscovita detrítica, fragmento de rocha pelítica, metamórfica e chert e raros bioclastos. O cimento é de calcita espática não ferrosa, óxido/hidróxido de ferro e sobrecrescimento de sílica. A porosidade é intergranular, móldica e às vezes alongada, sem permeabilidade perfazendo até 11% da rocha. Os processos diagenéticos dos arenitos são compactação física, sobrecrescimento de sílica, cimentação de calcita, formação de matriz diagenética, compactação química, substituição de grãos, autigênese de pirita, formação de óxido/hidróxido de ferro e alteração do plagioclásio. Os processos diagenéticos dos carbonatos são: micritização, neomorfismo, colomitização, fraturamento, compactação química, cimentação de calcita, dissolução secundária e autigênese de minerais. A sucessão da Formação Itaituba representa um sistema de laguna/planície de maré ligada a uma plataforma marinha carbonática. Planícies de maré desenvolveram-se nas margens das lagunas e eram periodicamente supridas por influxos de terrígenos finos (silte) que inibiam a precipitação carbonática. Barras bioclásticas eram cortadas por canais de maré (inlet) que conectavam a laguna com a plataforma rasa rica em organismos bentônicos.

Ground penetrating radar (GPR) and electrical resistivity tomography (ERT) survey on the neotectonic activity of the Padul-Nigüelas Fault Zone (PNFZ), Southern Spain

The Padul-Nigüelas Fault Zone (PNFZ) is situated at the south-western mountain front of the Sierra Nevada (Spain) in an extensive regime and belongs to the internal zone of the Betic Cordilleras. The aim of this study is a collection of new evidence for neotectonic activity of the fault zone with classical geological field work and modern geophysical methods, such as ground penetrating radar (GPR). Among an apparently existing bed rock fault scarp with triangular facets, other evidences, such as deeply incised valleys and faults in the colluvial wedges, are present in the PNFZ. The preliminary results of our recent field work have shown that the synsedimentary faults within the colluvial sediments seem to propagate basinwards and the bed rock fault is only exhumed due to erosion for the studied segment (west of Marchena). We will use further GPR data and geomorphologic indices to gather further evidences of neotectonic activity of the PNFZ.

Experimentally induced diesel engine injector faults and some preliminary acoustic emission signal observations

Diesel engine fuel injector faults can lead to reduced power, increased fuel consumption and greater exhaust emission levels and if left unchecked, can eventually lead to premature engine failure. This paper provides an overview of the Diesel, or compression ignition combustion process, and of the two basic fuel injector nozzle designs used in Diesel engines, namely, the pintle-type and hole-type nozzles. Also described are some common faults associated with these two types of fuel injector nozzles and the techniques previously used to experimentally simulate these faults. This paper also presents a recent experimental campaign undertaken using two different diesel engines whereby various fuel injector nozzle faults were induced into the engines. The first series of tests was undertaken using a turbo-charged 5.9 litre; Cummins Diesel engine whist the second series of tests was undertaken using a naturally aspirated 4 cylinder, 2.216 litre, Perkins Diesel engine. Data corresponding to different injector fault conditions was captured using in-cylinder pressure, and acoustic emission transducers along with both crank-angle encoder and top-dead centre reference signals. Using averaged in-cylinder pressure signals, it was possible to qualify the severity of the faults whilst averaged acoustic emission signals were in turn, used as the basis for wavelets decomposition. Initial observations from this signal decomposition are also presented and discussed.

Condition monitoring and diagnosis of injector faults in a diesel engine using in-cylinder pressure and acoustic emission techniques

Failing injectors are one of the most common faults in diesel engines. The severity of these faults could have serious effects on diesel engine operations such as engine misfire, knocking, insufficient power output or even cause a complete engine breakdown. It is thus essential to prevent such faults from occurring by monitoring the condition of these injectors. In this paper, the authors present the results of an experimental investigation on identifying the signal characteristics of a simulated incipient injector fault in a diesel engine using both in-cylinder pressure and acoustic emission (AE) techniques. A time waveform event driven synchronous averaging technique was used to minimize or eliminate the effect of engine speed variation and amplitude fluctuation. It was found that AE is an effective method to detect the simulated injector fault in both time (crank angle) and frequency (order) domains. It was also shown that the time domain in-cylinder pressure signal is a poor indicator for condition monitoring and diagnosis of the simulated injector fault due to the small effect of the simulated fault on the engine combustion process. Nevertheless, good correlations between the simulated injector fault and the lower order components of the enveloped in-cylinder pressure spectrum were found at various engine loading conditions.

Diesel engine problems, acoustic emission signals and simulated misfire faults

This paper discusses commonly encountered diesel engine problems and the underlying combustion related faults. Also discussed are the methods used in previous studies to simulate diesel engine faults and the initial results of an experimental simulation of a common combustion related diesel engine fault, namely diesel engine misfire. This experimental fault simulation represents the first step towards a comprehensive investigation and analysis into the characteristics of acoustic emission signals arising from combustion related diesel engine faults. Data corresponding to different engine running conditions was captured using in-cylinder pressure, vibration and acoustic emission transducers along with both crank-angle encoder and top-dead centre signals. Using these signals, it was possible to characterise the diesel engine in-cylinder pressure profiles and the effect of different combustion conditions on both vibration and acoustic emission signals.

Compaction control of topography and fault network structure along strike-slip faults in sedimentary basins

Strike-slip faults commonly display structurally complex areas of positive or negative topography. Understanding the development of such areas has important implications for earthquake studies and hydrocarbon exploration. Previous workers identified the key factors controlling the occurrence of both topographic modes and the related structural styles. Kinematic and stress boundary conditions are of first-order relevance. Surface mass transport and material properties affect fault network structure. Experiments demonstrate that dilatancy can generate positive topography even under simple-shear boundary conditions. Here, we use physical models with sand to show that the degree of compaction of the deformed rocks alone can determine the type of topography and related surface fault network structure in simple-shear settings. In our experiments, volume changes of ∼5% are sufficient to generate localized uplift or subsidence. We discuss scalability of model volume changes and fault network structure and show that our model fault zones satisfy geometrical similarity with natural flower structures. Our results imply that compaction may be an important factor in the development of topography and fault network structure along strike-slip faults in sedimentary basins.

The detection of incipient faults in small multi-cylinder diesel engines using multiple acoustic emission sensors

This thesis investigates condition monitoring (CM) of diesel engines using acoustic emission (AE) techniques. The AE signals recorded from a small size diesel engine are mixtures of multiple sources from multiple cylinders. Thus, it is difficult to interpret the information conveyed in the signals for CM purposes. This thesis develops a series of practical signal processing techniques to overcome this problem. Various experimental studies conducted to assess the CM capabilities of AE analysis for diesel engines. A series of modified signal processing techniques were proposed. These techniques showed promising results of capability for CM of multiple cylinders diesel engine using multiple AE sensors.