The North Cycladic Detachment System     

Laurent Jolivet  Emmanuel Lecomte  Benjamin Huet  Yoann Denèle  Olivier Lacombe  Loïc Labrousse  Laetitia Le Pourhiet  Caroline Mehl 《Earth and Planetary Science Letters》2010,289(1-2):87-104

Low-angle normal faults accommodate a large part of continental post-orogenic extension. Besides the intrinsic rheological characteristics of the continental crust that may lead to the formation of shallow-dipping shear zones at the brittle–ductile transition, the role of pre-existing low-angle structures such as large thrusts has been proposed by several authors. We explore this question with the example of the North Cycladic Detachment System (NCDS) that is composed of a series of distinct detachments cropping out on the islands of Andros, Tinos and Mykonos, separating the Cycladic Blueschists in the footwall from the Upper Cycladic Nappe in the hanging wall. We show that these extensional structures are part of a single large-scale structure (more than 200 km along strike) that reactivates the Vardar suture zone. It extends eastward on Ikaria and westward offshore Evia and Thessalia where it probably connects to recent shallow-dipping normal faults evidenced on published seismic reflection profiles. The NCDS started its activity in the Oligocene concommitantly with the Aegean extension, and was still active in the Late Miocene. It has exhumed a series of metamorphic domes from southern Evia to Mykonos below low-angle detachment systems, made of low-angle normal faults and low-angle ductile shear zones. The ductile shear zones and the faults were created with a low dip and they kept the same attitude throughout their exhumation. We identify three main detachments that are part of a continuum of extension on the NCDS : Tinos detachment, Livada detachment and Mykonos detachment. A fourth detachment (Vari detachment) is the reactivation of an Eocene exhumation-related structure. Deformation in the footwall is characterized by intense stretching and flattening. Using the spatial evolution observed along strike from Andros to Mykonos we construct a history of formation of the NCDS starting with the reactivation of former thrusts leading to the exhumation of high-temperature metamorphic domes. The Aegean example shows that reactivation of earlier shallow-dipping discontinuities can play a fundamental role in continental post-orogenic extension.  相似文献   

The Meteoritical Bulletin,No. 95     

Michael K. WEISBERG  Caroline SMITH  Gretchen BENEDIX  Luigi FOLCO  Kevin RIGHTER  Jutta ZIPFEL  Akira YAMAGUCHI  Hasnaa CHENNAOUI AOUDJEHANE 《Meteoritics & planetary science》2009,44(3):429-462

  相似文献   

Multiple Tuned Mass Damper Based Vibration Mitigation of Offshore Wind Turbine Considering Soil–Structure Interaction   总被引：1，自引：0，他引：1  

Mosaruf Hussan  Faria Sharmin  Dookie Kim 《中国海洋工程》2017,31(4):476-486

The dynamics of jacket supported offshore wind turbine(OWT) in earthquake environment is one of the progressing focuses in the renewable energy field. Soil–structure interaction(SSI) is a fundamental principle to analyze stability and safety of the structure. This study focuses on the performance of the multiple tuned mass damper(MTMD) in minimizing the dynamic responses of the structures objected to seismic loads combined with static wind and wave loads. Response surface methodology(RSM) has been applied to design the MTMD parameters. The analyses have been performed under two different boundary conditions: fixed base(without SSI) and flexible base(with SSI). Two vibration modes of the structure have been suppressed by multi-mode vibration control principle in both cases. The effectiveness of the MTMD in reducing the dynamic response of the structure is presented. The dynamic SSI plays an important role in the seismic behavior of the jacket supported OWT, especially resting on the soft soil deposit.Finally, it shows that excluding the SSI effect could be the reason of overestimating the MTMD performance.  相似文献   

Pyrite oxidation during sample storage determines phosphorus fractionation in carbonate-poor anoxic sediments   总被引：4，自引：0，他引：4  

Peter Kraal  Caroline P. Slomp  Marcel M.M. Kuypers 《Geochimica et cosmochimica acta》2009,73(11):3277-3290

We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (∼94 Ma) and the Paleocene-Eocene thermal maximum (∼55 Ma), that were exposed to oxygen after core recovery. Surprisingly, P associated with iron oxyhydroxides (Fe-bound P) was a major P phase in these laminated sediments deposited under euxinic conditions. A significant fraction of total Fe was present as (poorly) crystalline ferric Fe. This fraction increased with increasing storage time of the investigated cores. In carbonate-poor samples, Fe-bound P accounted for up to 99% of total P and its abundance correlated with pyrite contents. In samples with higher CaCO₃ contents (>5 wt% in the investigated samples), P was mostly present in authigenic Ca-P minerals, irrespective of pyrite contents. We conclude that the P fractionation in anoxic, carbonate-poor, sediments is strongly affected by pyrite oxidation that occurs when these sediments are exposed to oxygen. Pyrite oxidation produces sulfuric acid and iron oxyhydroxides. The abundance of poorly crystalline Fe oxyhydroxides provides further evidence that these were indeed formed through recent (post-recovery) oxidation rather than in situ tens of millions of years ago. The acid dissolves apatite and the released phosphate is subsequently bound in the freshly formed iron oxyhydroxides. Pyrite oxidation thus leads to a conversion of authigenic Ca-P to Fe-bound P. In more calcareous samples, CaCO₃ can act as an effective buffer against acidic dissolution of Ca-P minerals. The results indicate that shielding of sediments from atmospheric oxygen is vital to preserve the in situ P fractionation and to enable a valid reconstruction of marine phosphorus cycling based on sediment records.  相似文献   

Physiochemical controls on the crystal-chemistry of Ni in birnessite: Genetic implications for ferromanganese precipitates     

Caroline L. Peacock 《Geochimica et cosmochimica acta》2009,73(12):3568-6415

Sorption of Ni to birnessite is a fundamental control on the concentration of Ni in natural waters and associated sediments. Recent XAS work suggests the crystal-chemistry of Ni in birnessite is dependent on both structural and physiochemical factors. This work investigates the physiochemical controls on Ni crystal-chemistry in hexagonal birnessite with EXAFS of time series and pH series Ni-birnessite sorption experiments. At circumneutral pH Ni surface adsorbed above/below Mn octahedral vacancy sites in the phyllomanganate layers is progressively structurally incorporated into the vacancy sites with time (30% Ni incorporation after 408 h contact time). Ni structural incorporation into hexagonal birnessite occurs via rearrangement of surface adsorbed Ni with time rather than direct Ni incorporation from solution. At low pH (pH 4) Ni surface adsorbed at the vacancies is structurally incorporated into the vacancies upon increasing solution pH to circumneutral (∼20% Ni incorporation after 24 h contact time at circumneutral pH); newly incorporated Ni is stable with increasing contact time at pH circumneutral. However, upon decreasing solution pH from circumneutral back to pH 4, EXAFS shows a significant decrease in the proportion of Ni structurally incorporated; preliminary results indicate structural incorporation of Ni in hexagonal birnessite is reversible with decreasing pH. Time series results at circumneutral pH help explain the significant enrichment of Ni in marine ferromanganese precipitates; work here is combined with previous studies to provide a model correct at the molecular-level for Ni uptake by marine vernadite-rich ferromanganese precipitates. With Ni migrating from surface adsorbed to structurally incorporated, results suggest formation of a solid solution between an end-member vernadite and an end-member Ni-vernadite phase, with surface adsorption acting as a mechanism of transition from one composition to the other. pH series results call into question the viability of Ni crystal-chemistry in natural vernadite as a paleo-proxy for paleo-pH conditions in freshwater systems and challenge the traditional view that structurally incorporated trace-metals are stable within the Eh-pH field of the host mineral phase. Natural birnessite may not be as permanent a sink for Ni as first suggested by Ni crystal-chemistry.  相似文献   

Ordovician magmatism in the Lévézou massif (French Massif Central): tectonic and geodynamic implications     

Lotout  Caroline  Pitra  Pavel  Poujol  Marc  Van Den Driessche  Jean 《International Journal of Earth Sciences》2017,106(2):501-515

International Journal of Earth Sciences - New U–Pb dating on zircon yielded ca. 470 Ma ages for the granitoids from the Lévézou massif in the southern French Massif...  相似文献   

Brazilian Solar Spectroscope (bss)     

Sawant  H.S.  Subramanian  K.R.  Faria  C.  Fernandes  F.C.R.  Sobral  J.H.A.  Cecatto  J.R.  Rosa  R.R.  Vats  H.O.  Neri  J.A.C.F.  Alonso  E.M.B.  Mesquita  F.P.V.  Portezani  V.A.  Martinon  A.R.F. 《Solar physics》2001,200(1-2):167-176

Digital, decimetric (200–2500 MHz) Brazilian Solar Spectroscope (BSS) with high time (10–1000 ms) and frequency (1–10 MHz) resolution is in regular operation since April, 1998, at National Space Research Institute (INPE) at São José dos Campos, Brazil. BSS operates in conjunction with a 9-m diameter polar mounted antenna. It allows to select suitable observing frequency range, frequency and time resolutions and data can be digitized up to 100 channels. BSS has capabilities of quasi-real time display of the ongoing dynamic spectra of the solar activity that enables the observer to modify observational parameters so as to suit a specific type of activity such as spikes and improve the quality of data acquisition and storage. Minimum detectable flux density of the spectroscope, for different combinations of the observational parameters, is 3 s.f.u. Observations are carried out routinely from 11 UT to 19 UT. Necessary software for data acquisition and reductions has been developed in IDL 5.3 environment. Data are available in FITS and ASCII formats. Absolute timing accuracy of the station is less than 3 ms. Here, we present examples of the bursts which have been recorded by BSS and available display facilities.  相似文献   

Seismic evaluation of concrete dams via continuum damage models     

Miguel Cervera  Javier Oliver  Rui Faria 《地震工程与结构动力学》1995,24(9):1225-1245

In this paper a general methodology for the analysis of large concrete dams subjected to seismic excitation is outlined. It is valid both for gravity dams (2D representation) and arch dams (3D representation). The method allows for non-linear material behaviour of the dam, ‘transparent fictitious boundaries’ for dealing properly with in-coming and out-going seismic waves, and an efficient procedure to deal with dam-soil-fluid interaction. The mechanical behaviour of concrete is modelled using an isotropic damage model which allows for tension and compression damage, and exhibits stiffness recovery upon load reversals. Emphasis is placed in the treatment of fluid-structure interaction, regarding both formulation and efficiency aspects. A gravity dam and an arch dam are analysed subjected to artificially generated earthquakes of different intensities, and the results are used to study the degree of (un)safety of the dams.  相似文献   

Sublethal and lethal effects of sediments applied to common Caribbean Reef corals in the field     

Caroline S Rogers 《Marine pollution bulletin》1983,14(10):378-382

Experiments to measure natural rates of sedimentation and to assess the tolerance of coral species to increased sedimentation were conducted at San Cristobal Reef, Puerto Rico. Sedimentation rates were measured over an 18 month period. Calcareous sediments were applied to colonies of Montastraea annularis, Diploria strigosa, D. clivosa, Acropora palmata and A. cervicornis in different frequencies and in different doses.Mean sedimentation rates from sediment traps were 9.6±2.4 (S.E.) mg cm^?2 · day^?1 at 10 cm above the bottom and 2.5±0.9 (S.E.) and 2.6±1.2 (S.E.) mg cm^?2 · day^?1 for two sets of traps at 50 cm above the bottom. Sediment application experiments indicated A. palmata was the least tolerant of the species tested. Although A. cervicornis and D. strigosa colonies were not significantly affected, single applications of 800 mg cm^?2 to M. annularis colonies and of 200 mg cm^?2 to A. palmata colonies caused death of underlying coral tissue. Algae colonized the smothered portions of these corals.  相似文献   

From granitoid to kyanite-bearing micaschist during fluid-assisted shearing (Ile d’Yeu, France)     

Caroline Sassier  Philippe Boulvais  Denis Gapais  Ramon Capdevila  Hervé Diot 《International Journal of Earth Sciences》2006,95(1):2-18

We describe amphibolite-facies shear zones affecting an orthogneiss from the Armorican Hercynian belt (Ile d’Yeu, western France). The deformation pattern is consistent with top-to-the-South thrusting followed by E–W extension, as documented elsewhere in the region. Shearing was accompanied by channelled fluid flow that transformed the orthogneiss into a peraluminous micaschist. Structural and mineralogical data indicate rather early strain localization. Then, temperature increase associated with crustal thickening favoured more distributed deformations marked by shear zone stretching and the development of a HT regional foliation. Chemical analyses made across five shear zones show mass transfers that mainly implied losses in Ca and Na, and gains in H₂O, Mg, and K. Most results indicate constant volume transformation, but some suggest records of either gains or losses of volume (between +20% and −30%). This might reflect variable records of fluid-rock interactions according to the timing of initiation and subsequent evolution of individual shear zones, early thrusting stages being marked by up-temperature flow, and late thrusting stages by down-temperature flow. δ¹⁸O analyses suggest that fluids experienced significant isotopic exchange with orthogneisses.  相似文献