兰州-民和盆地红古城组的建立及其地质学意义   总被引：7，自引：0，他引：7  

蔡雄飞  朱伟元 《甘肃地质》1998,7(2):49-53

兰州—民和盆地下白垩统地层,出露良好,厚度较大,自下而上可建立８个非正式的岩石地层单位（岩组）。红古城组位于下白垩统上部的第七岩组。该组以剖面连续、出露甚好、顶底清楚、厚度不大而与上、下地层显著不同,具独特的岩性、岩相特征。虽然岩性、岩相在横向上变化较快,但顶、底界线都具良好的标志层,在盆地内可以广泛追索和对比。该组岩石地层单位的正式建立,不仅便于区内地层的划分与对比,而且对盆内层序地层、岩相分析、构造演化的研究都具重要意义。  相似文献   

中原末次冰期间冰阶以来的古季风气候变迁   总被引：6，自引：2，他引：4  

肖华国  吴锡浩  蒋复初  田国强  刘科  薛滨  孙东怀 《地球学报》1998,19(1):84-89

中原邙山黄土地层以巨厚的马兰黄土为特色。本文研究了末次冰期间冰阶以来邙山黄土－古土壤序列的粗颗粒含量和磁化率值曲线反映的冬夏季风变迁及其相互关系,发现在万年尺度上夏季风增强对应于冬季风减弱,冬季风增强对应于夏季风减弱,但在千年尺度上冬季风变化比夏季风强烈得多,而且末次间冰段开始时冬季风减弱明显早于夏季风增强。通过中原黄土记录与深海及冰芯Ｏ同位素记录的对比,发现短时间尺度气候变化阶段明显具有很大的区域性特征,它们不能简单地进行等时性全球对比,而应该通过各自独立的时间标尺来建立古气候变化的远距离联系。  相似文献   

The effect of the temporal resolution of the wind forcing on a central Mediterranean Sea model     

《Dynamics of Atmospheres and Oceans》2021

The impact of the wind forcing temporal resolution in the central Mediterranean Sea is addressed using a numerical ocean circulation model. The model uses interactive surface fluxes based on the ERA-Interim 6-hourly atmospheric reanalyses except for the 10 m wind for which ERA5 hourly reanalyses are used. Additional temporal resolution (2, 3, 6, 12 and 24 h) wind sets are deduced from the ERA5 hourly data. An ensemble of simulations (six members) is then performed where only the temporal resolution of the wind forcing is changed. The impact of the temporal resolution is studied based on this set of simulations. The dependence of the surface wind stress and heat flux on the wind resolution is derived based on an analytical expression where the Weibull distribution is used to characterise the probability density function of the wind speed. Results from the analytical model are found close to those from the numerical model when a linear increase of the exchange coefficients with the wind speed is considered. Power input into the sea and surface heat loss both increase with the increase of the temporal resolution but at lower rates when approaching hourly forcing values. The increase of the latent heat loss at these high resolutions is small (~−0.8 Wm^-2) but still important, around 10–20% the Mediterranean basin heat budget (−5 to −7 Wm^-2). The increase of the wind forcing temporal resolution decreases the sea surface temperature (SST) and increases the sea surface salinity (SSS) with largest values in the shallow area of the Gulf of Gabès (eastern coast of Tunisia). A decrease of SSS is however noticed in some areas mainly northwest of the Tunisia coast. Hydrographical changes are also found in the Tunisia-Sicily channel. They are characterised by mesoscale structures with no remarkable change of the major water veins.  相似文献   

A Jurassic garnet-bearing granitic pluton from NE China showing tetrad REE patterns   总被引：16，自引：0，他引：16  

Fu-yuan Wu  De-you Sun  Bor-ming Jahn  S. Wilde 《Journal of Asian Earth Sciences》2004,23(5):731-744

NE China is characterized by the massive distribution of Phanerozoic granitoids. Most of them are of I- and A-type granites, whereas S-type granites are rarely documented. The present work deals with the Dongqing pluton, a small granitic body emplaced in the southern Zhangguangcai Range. The pluton comprises a two-mica (±garnet) granite and a garnet-bearing muscovite granite; the latter occurs as veins in the former. The pluton shows a gradational contact with the surrounding host granites. Rb–Sr and Sm–Nd isotope analyses on whole-rocks and minerals reveal that the two types of granites were emplaced synchronously at about 160 Ma. The pluton was emplaced coeval with the surrounding I-type granitic pluton, and had a rapid cooling history. It is characterized by an initial Sr isotopic ratio of 0.706, slightly negative _Nd(T) values (−0.5 to −1.9) and young depleted-mantle model ages (970–1090 Ma). This suggests that the parent magma originated from partial melting of relatively juvenile crust, which is largely compatible with the general scenario for much of the Phanerozoic granitoids emplaced in the Central Asian Orogenic Belt.Geochemically, the granites of the Dongqing pluton are peraluminous, with a Shand Index (molar ratio A/CNK) of 1.0–1.1 for the two-mica granites and 1.2–1.3 for the garnet-bearing granites. All the garnet-bearing granites and some of the two-mica granites show tetrad REE patterns (=tetrad group), whereas most two-mica granites show normal granitic REE patterns (=normal group). The normal group granites exhibit depletion in Nb, Ta, P and Ti in spidergrams, and generally weak positive Eu anomalies in REE patterns. By contrast, the tetrad group granites manifest depletion in Ba, Nb, Ta, Sr, P, and Ti and significant negative Eu anomalies. The trace element data constrain the parental magmas to having undergone extensive magmatic differentiation. During their late stage magmatic evolution, intense interaction of residual melts with aqueous hydrothermal fluids resulted in the non-CHARAC (charge and radius controlled) trace element behavior and the tetrad effect in REE distribution patterns. This, in turn, leads to the invalidation of the commonly used tectonic discrimination criteria derived from trace element abundances of normal granites. In view of this and previous studies, we conclude that there were probably no S-type granites produced in NE China during the Phanerozoic. Consequently, weathered sedimentary material did not play an important role in the genesis of the strongly peraluminous granites in the Zhangguangcai Range.  相似文献   

Electronically conducting brittle-ductile shear zones in the crystalline basement of Rittsteig (Bohemian Massif,Germany): Evidence from self potential and hole-to-surface electrical measurements     

Jürgen?Bigalke  Andreas?Junge  Gernold?ZulaufEmail author 《International Journal of Earth Sciences》2004,93(1):44-51

Crustal-scale shear zones may act as prominent electrical conductors given that sufficient amounts of graphite or fluids are present. There are several graphite-enriched shear zones within the 583-m-deep Rittsteig drilling (Bavaria, Germany), two of which are of major importance. One shear zone cuts through Moldanubian biotite-muscovite schists at 320 m depth. The other shear zone separates Teplá-Barrandian amphibolites from Moldanubian biotite-muscovite schists at 460 m depth. To detect these shear zones adjacent to the drilling, the self-potential method and the non-linear impedance spectroscopy have been applied. From the new data, obtained from hole-to-surface and surface measurements, we conclude that (1) graphite is pervasively distributed within the Rittsteig shear zones resulting in powerful electronic conductors, (2) the graphite-bearing shear zones are dipping moderately towards the S, and (3) the shear zone drilled at 320 m depth extends to the Earths surface where it has been detected ca. 400 m to the N of the drilling. As the graphite-bearing shear zones of both the Rittsteig drilling and the German Continental Deep Drilling (KTB) developed in the brittle-ductile regime of quartzofeldspathic rocks, we argue that the brittle-ductile boundary layer may act as a significant graphite attractor in the continental crust.

Gernold ZulaufEmail: Phone: +49-9131-8522617Fax: +49-9131-8529295

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Mio-Pliocene basin development in the eastern part of the Cappadocian Volcanic Province (Central Anatolia,Turkey) and its implications for regional tectonics     

Faruk?Ocako?luEmail author 《International Journal of Earth Sciences》2004,93(2):314-328

The Cappadocian Volcanic Province (CVP) comprises predominantly of a thick succession of volcanogenic rocks and interbedded siliciclastic sediments of Middle Miocene to Recent age in Central Anatolia, Turkey. The conditions of basin development in the eastern part of the CVP have been elucidated by using sedimentological and geomorphological approaches. The prevailing tectonic regime, its extent and causes are also discussed. Sedimentological analysis supported by geomorphological observations revealed a major NE-trending probably normal, border fault and its several synthetics. This tectonic element constitutes the SE margin of the basin and divided the CVP from the Tauride range during Middle Miocene to Pliocene. The basin fill in the study area comprises gravelly alluvial fans near the border fault, while fluvial clastics and lacustrine carbonates dominate towards the centre. Some pyroclastic rocks and lava flows are also made part of the fill. The southeastern basin margin is characterized morphologically by a number of uplifted basement blocks, probably associated with synthetic faults, and some deeply incised canyons in the footwall. These canyons were subsequently filled with a Mid-Pliocene ignimbrite sheet, and represent the sediment supply conduits to the basin. The cessation of filling in the basin was determined by strike-slip faults that uplifted and detached the basin about 2.6 Ma. This date also marks the onset of the neotectonic period in the region. The overall extensional tectonic regime inferred for the eastern CVP appears coeval with events recognised in the southern basins, i.e. Adana and Mut Basins and the eastern Mediterranean. Some physical connections between these basins also have been demonstrated. It is suggested that the CVP and the southern basins were all created during a phase of extension resulting from continued northward subduction of the African plate beneath the Eurasia during the Late Cenozoic.  相似文献   

Tectonic evolution of the internal sector of the Central Apennines, Italy   总被引：2，自引：0，他引：2  

F. Sani  C. Del Ventisette  D. Montanari  M. Coli  P. Nafissi  A. Piazzini 《Marine and Petroleum Geology》2004,21(10):1235-1254

A wide sector of the internal portion of the Central Apennines, which comprises the southern Lepini Mtns up to the northern Simbruini Mtns has been investigated through detailed field mapping and integrated with structural analyses. A few small productive oil fields and a large number of hydrocarbon seeps and oil impregnations are located in this sector. This area offers good opportunities for testing the use of structural fieldwork methodologies in order to highlight oil migrating paths, from Triassic source rocks, and prospecting chances for oil field exploitation.The main stages of the structural evolution of the area took place after deposition of the foredeep sediments (Frosinone Fm.), i.e. after Late Tortonian, under a stress field characterised by a NE–SW trending σ₁, which was responsible for the early emplacement of major thrust faults present in the area. The Messinian-Early Pliocene thrust-top basin deposits allowed the reconstruction of an in-sequence evolution of the thrust system. The development of out-of-sequence thrusting post-dates these structures leading to a further strong shortening phase in the area during the Pliocene. This phase is characterised by a roughly NNE–SSW trending σ₁. Some peculiar tectonic features evidenced by thrust faults with younger-over-older relationships and an inversion of the original stacking of thrust sheets developed during this phase.Successively, a block-faulting tectonic, mainly with NE–SW extension stress field, occurred and dismembered the compressive tectonic edifice.Later on up to the Middle Pleistocene, N–S to NNE–SSW trending dextral strike-slip faults also acted in the area. Associated to the strike-slip tectonics are local volcanic centres as well as necks, whose compositions show a mantle origin, thus indicating deep seating and a possible lithospheric significance of these structures.In the light of this study, the reduced extension of the productive oil area as well as the spotting of oil seeps, may indicate that the migration conditions are not tied to well defined structures but that likely the cross-cutting points among structures facilitate the conditions for an upwards rising of oil. These conditions in particular are achieved at least in two cases: (1) where the Late Triassic source rocks do not have great depth due to normal or reverse faults, or (2) at a major depth when encountered by transcurrent-oblique roughly N–S trending faults—in both cases oil can easily migrate along the damage zone associated to the fault plane.  相似文献   

Seabird distribution on the Humboldt Current in northern Chile in relation to hydrography, productivity, and fisheries     

Weichler  Tanja; Garthe  Stefan; Luna-Jorquera  Guillermo; Moraga  Julio 《ICES Journal of Marine Science》2004,61(1):148-154

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A review of the impacts of salmonid farming on marine coastal ecosystems in the southeast Pacific   总被引：2，自引：0，他引：2  

Buschmann  Alejandro H.; Riquelme  Veronica A.; Hernandez-Gonzalez  Maria C.; Varela  Daniel; Jimenez  Jaime E.; Henriquez  Luis A.; Vergara  Pedro A.; Guinez  Ricardo; Filun  Luis 《ICES Journal of Marine Science》2006,63(7):1338-1345

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Direct barite determination using SEM/EDS-ACC system: implication for constraining barium carriers and barite preservation in marine sediments     

E. Robin  C. Rabouille  G. Martinez  I. Lefevre  J. L. Reyss  P. van Beek  C. Jeandel 《Marine Chemistry》2003,82(3-4):289-306

Barite (BaSO₄) in marine sediments is considered as a proxy of surface ocean productivity and is widely used for paleo-productivity reconstructions. However, direct barite determination is not achieved by currently used methods, which rely on the measurement of total barium by inductively coupled plasma–mass spectrometry (ICP-MS) and instrumental neutron activation analysis (INAA) and correction from the allogenic Ba contribution. We report here on a technique that directly counts individual barite crystals using a scanning electron microscope (SEM) coupled to an energy dispersive spectrometer (EDS) equipped with an automated particle counting and classification (ACC) system. We show that barite–Ba concentrations can be deduced from the abundance, shape and size distributions of barite crystals with current precision and sensitivity as high as ±5 wt.% (2σ confidence limit) and 10 ppm, respectively. This technique, coupled with ICP-MS and INAA techniques for total Ba measurements, was applied to sediment samples from the tropical North Atlantic and the Central North Pacific oceans. Results show that: (1) barite and detrital aluminosilicates are the two main carriers of Ba in the investigated sediments; (2) calculated Ba/Al ratios range from 0.005 to 0.008 with an average value around 0.0066, in close agreement with previously reported values; (3) barite might not be the major source for released barium out of sediments and we suggest instead adsorbed barium as a potential source.  相似文献