Geology and geochemistry of Jurassic pelagic sediments, Scisti silicei Formation, southern Apennines, Italy     

Paola Di Leo  Enrico Dinelli  Giovanni Mongelli  Marcello Schiattarella 《Sedimentary Geology》2002,150(3-4):229-246

A better understanding of genesis and palaeoenvironmental setting of the Scisti silicei Formation (Lagonegro units, southern Italy) was achieved by means of geochemical analysis integrated with new stratigraphic information. Data show that major and trace element geochemistry of ancient clay-rich beds and banded cherts add new insights into the Mesozoic evolution of the Lagonegro basin. Sedimentary contributions to Jurassic shales sampled during this study were mainly derived from two major sources: (i) a dominant terrigenous fine-grained component, having affinity with average upper continental crust that had not undergone intense weathering and (ii) biogenic siliceous material. The latter component occurs in clay-rich layers from the “basal member” of the Scisti silicei Formation.

Composition varies up section and accounts for changes in the detrital supply due to bathymetric oscillations. The compositional variations from the basal to the overlying member are consistent with a distal source passing in time to a more “proximal” source, as indicated by sharp changes in the concentrations of detrital elements (Ti, Zr and Nb). It is likely that increased detrital input occurred through turbidity current deposition. Finally, the chemical features of the clay-rich layers from the upper cherty portion of the studied succession imply a progressive deepening of the basin.

The lack of any mafic and hydrothermal contributions in the Jurassic shales as well as the continental nature of detrital input suggests that the Lagonegro basin was located between two carbonate platforms, in accordance with the classical restoration of the African–Apulian palaeomargin. Thus, the basin acted as a preferential sink connected to the African cratonic areas through a southern entry point.  相似文献   

Post-seismic relaxation and earthquake triggering in the southern Adriatic region   总被引：1，自引：0，他引：1  

Marcello Viti  Francesca D'Onza  Enzo Mantovani  Dario Albarello  Nicola Cenni 《Geophysical Journal International》2003,153(3):645-657

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干旱区间歇性河流河道两侧地下水运动模型及其求解方法     

阿曼吐尔·哈力克 《地下水》2008,30(5):9-11

由于上中游水资源的过多开发利用,我国西北干旱区有些内陆河下游来水量急剧减少,从以前的常年性河流逐渐转变成现在的间歇性河流,给当地带来了一系列严重的生态环境问题。根据间歇性河流河道充水和停水过程周期性重复出现的水文特征,建立了河道两侧区域地下水运动的一维非稳定流模型,提出了把流量边界条件与水位界条件相互转换来求解模型的一种方法。最后应用上述模型分析西北某内陆河下游间歇性输水条件下河道两侧地区地下水位恢复状况,为输水生态效应的定量评价提供了理论基础。  相似文献   

新疆阿勒泰驼峰山地震台水管倾斜、洞体应变观测异常核实     

时显军  邢喜民  叶尔扎提·巴合提汗 《地震地磁观测与研究》2020,41(4):143-147

2013年以来,阿勒泰驼峰山地震台水管倾斜、洞体应变观测值同步趋势性变化,经核实,将其作为学科的A类趋势性异常进行跟踪。在该趋势性异常的背景下,伸缩仪于2018年10月20日起,水管倾斜仪11月24日起,NS分量出现不明原因的转向异常现象。针对该异常变化,于2019年1月1日开展异常核实,认为：①水管倾斜仪工作稳定,观测数据真实可靠;②2018年10月以来水管倾斜仪、伸缩仪观测数据的快速变化与气象要素基本无关,可能与驼峰山台正南方1.1 km处阿勒泰地区检察院对面酒店地下停车场土石方挖倔有较大关系。  相似文献   

Climatology of dust days in the Central Plateau of Iran     

Mesbahzadeh  Tayyebeh  Salajeghe  Ali  Sardoo  Farshad Soleimani  Zehtabian  Gholamreza  Ranjbar  Abbas  Krakauer  Nir Y.  Miglietta  Mario Marcello  Mirakbari  Maryam 《Natural Hazards》2020,104(2):1801-1817

Natural Hazards - Dust storms are a major natural hazard to human health. Severe erosive storms in parts of the Central Plateau of Iran have made the situation very difficult for the inhabitants,...  相似文献   

基于à trous小波分解的SAR图像噪声滤除方法   总被引：1，自引：1，他引：0  

文艳  丁建丽  塔西甫拉提·特依拜 《测绘科学》2009,34(1)

合成孔径雷达(SAR)以其特有的全天时、全天候成像能力,在对地观测领域中发挥着重要的作用。由于雷达回波的相干性,SAR图像上存在着斑点噪声,为消除这种噪声,提出了一种基于à trous小波算法的组合滤波方法,该方法首先将SAR图像分解至静态小波域,然后对噪声的小波系数进行基于中值的平滑处理,最后对低频信号进行均值滤波。将此算法应用于新疆库车县的一幅RADARSAT图像进行斑点噪声滤波,并与另外3种典型的SAR图像滤波算法进行比较,结果表明,该方法不仅可以有效地去除斑点噪声,并且可以保持SAR图像的精细纹理结构。  相似文献   

Resolution dependent relative dispersion statistics in a hierarchy of ocean models     

Andrew C. Poje  Angelique C. Haza  Tamay M. Özgökmen  Marcello G. Magaldi  Zulema D. Garraffo 《Ocean Modelling》2010,31(1-2):36-50

In order to determine the effect of Eulerian spatial resolution on the two particle statistics of synthetic drifter trajectories, we examine a hierarchy of ocean models, starting from 2D turbulence simulations, progressing to idealized simulations of a buoyant coastal jet with ROMS, and finally to realistic HYCOM simulations of the Gulf Stream. In each case, particle dispersion at large time and space scales is found to be controlled by energetic meso-scale features of the flow that are relatively insensitive to the resolution of finer scale motions. In all cases, time-distance graphs given in terms of computed Finite Scale Lyapunov Exponents show an expected increase in the extent of exponential scaling with increasing spatial smoothing of the velocity field. The limiting value of the FSLE at small separation distances is found to scale remarkably well with the resolution of Eulerian velocity gradients as given by the average of positive Okubo–Weiss parameter values.  相似文献   

Layered amphibolite sequence in NE Sardinia,Italy: remnant of a pre-Variscan mafic silicic layered intrusion?     

Marcello?FranceschelliEmail author  Mariano?Puxeddu  Gabriele?Cruciani  Andrea?Dini  Marilisa?Loi 《Contributions to Mineralogy and Petrology》2005,149(2):164-180

A banded amphibolite sequence of alternating ultramafic, mafic (amphibolite) and silicic layers, tectonically enclosed within Variscan migmatites, outcrops at Monte Plebi (NE Sardinia) and shows similarities with leptyno-amphibolite complexes. The ultramafic layers consist of amphibole (75–98%), garnet (0–20%), opaque minerals (1–5%) and biotite (0–3%). The mafic rocks are made up of amphibole (65–80%), plagioclase (15–30%), quartz (0–15%), opaque minerals (2–3%) and biotite (0–2%). The silicic layers consist of plagioclase (60–75%), amphibole (15–30%) and quartz (10–15%). Alteration, metasomatic, metamorphic and hydrothermal processes did not significantly modify the original protolith chemistry, as proved by a lack of K₂O-enrichment, Rb-enrichment, CaO-depletion, MgO-depletion and by no shift in the rare earth element (REE) patterns. Field, geochemical and isotopic data suggest that ultramafic, mafic and silicic layers represent repeated sequences of cumulates, basic and acidic rocks similar to macrorhythmic units of mafic silicic layered intrusions. The ultramafic layers recall the evolved cumulates of Skaergaard and Pleasant Bay mafic silicic layered intrusions. Mafic layers resemble Thingmuli tholeiites and chilled Pleasant Bay mafic rocks. Silicic layers with Na₂O: 4–6 wt%, SiO₂: 67–71 wt% were likely oligoclase-rich adcumulates common in many mafic silicic layered intrusions. Some amphibolite showing a strong Ti-, P-depletion and REE-depletion are interpreted as early cumulates nearly devoid of ilmenite and phosphates. All Monte Plebi rocks have extremely low Nb, Ta, Zr, Hf content and high LILE/HFSE ratios, a feature inherited from the original mantle sources. The mafic and ultramafic layers show slight and strong LREE enrichment respectively. Most mafic layer samples plot in the field of continental tholeiites in the TiO₂–K₂O–P₂O₅ diagram and are completely different from N-MORB, E-MORB and T-MORB as regards REE patterns and Nd, Sr isotope ratios but show analogies with Siberian, Deccan and proto-Atlantic rift tholeiites. Comparisons with Thingmuli, Skaergaard and Kiglapait rocks and with experimental data suggest that the Monte Plebi intrusion was an open-to-oxygen system with fO₂ FMQ. Mafic and ultramafic samples yielded _Nd(460)=+0.79 /+3.06 and ⁸⁷Sr/⁸⁶Sr=0.702934–0.703426, and four silicic samples _Nd(460)=–0.53/–1.13; ⁸⁷Sr/⁸⁶Sr=0.703239–0.703653. Significant differences in Nd isotope ratios between mafic and silicic rocks prove that both groups evolved separately in deeper magma chambers, from different mantle sources, with negligible interaction with crustal material, and were later repeatedly injected within a shallower magma chamber. The spectrum of Sr and Nd isotope data is consistent with a slightly enriched mantle metasomatized during an event earlier than 460 Ma. The metasomatising component was represented by alkali-Th-rich fluids of crustal origin rather than by sedimentary materials, able to modify alkali and Sr–Nd isotope systematics. Monte Plebi layered amphibolites might represent the first example of a strongly metamorphosed fragment of an early Paleozoic mafic silicic layered intrusion emplaced in a thinning continental crust and then tectonically dismembered by Variscan orogeny.  相似文献   

Carbonate pseudotachylytes: evidence for seismic faulting along carbonate faults     

Alfio Viganò  Simone Tumiati  Sandro Recchia  Silvana Martin  Marcello Marelli  Riccardo Rigon 《地学学报》2011,23(3):187-194

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分布式水文模型SWAT模型在新疆叶尔羌河流域的适用性研究     

迈尔丹江·米吉提 《地下水》2015,(4)

为定量分析SWAT模型在新疆叶尔羌流域径流模拟的适用性,以叶尔羌河卡群水文站以上集水区域为研究流域,基于卡群水文站2000-2012年水文数据,运用SWAT模型模拟了研究流域的径流量,并设定2种气候变化情景模式,定量分析不同气候变化情景模式对叶尔羌流域径流量的影响。研究结果表明:SWAT模型在叶尔羌河流域具有较好的适用性,模拟的径流深相对误差小于8%,确定性系数均达到0.75以上;在降水不变化的前提下,气温升高2℃,流域径流量增加6.28%;在气温不变前提下,降水量增加5%,流域径流量增加9.50%。研究成果对于新疆叶尔羌河流域水文模拟及预测提供参考价值。  相似文献