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71.
本文报道由蓝田、陕县、洛川、西峰、平凉、兰州及靖远等剖面获得的古地磁研究结果.主要结论为:1.中国黄土剖面记录了Brunhes正极性带与Matuyama负极性带,Brunhes/Matuyama极性转换过程位于第8层黄土(L8).在段家坡黄土剖面该转换过程对应的地层厚度为0.375m,持续时间约6000a.转换过程由3次极性变化构成,每次经历的时间约为400a.2.Jaramillo正极性亚带(J)位于标志层L9至L15之间,大约S10-S13位置.3.Olduvai正极性亚带(O)对应的地层为S27-S334.Reunion正极性亚带(R)由两部分组成,在蓝田段家坡黄土剖面分别位于L36和S385.Matuyama负极性带与Gauss正极性带界限(M/Ga)位于黄土和红色粘土交界处,中国黄土的底界年龄为2.48Ma左右.黄土与红色粘土为整合接触关系.6.黄土下伏的红色粘土记录了Gauss正极性带,Gilbert负极性带和古地磁年表编号5(Epoch5). 相似文献
72.
Zhao-Yin WANG Yongsheng WU and Guangqian WANG Prof. Dept. of Hydraulic Engineering Tsinghua University & International Research Training Center on Erosion Sedimentation Beijing China Email: zywang@tsinghua.edu.cn or zywang@sun 《国际泥沙研究》2001,16(4)
1 mTRoorcnoxThe EnvirDment AgenCy of UK (l997) defins eUtIDPhication as "the enrichInnt of waters byinorgedc plant nUtrientS that result in the simulation of an mp Of syInPtOInati changes. These includethe inCrased PrOduCtiOn Of aigae or othe aquatic PlantS, affeChng the quallty of the water and distUIbingthe balance Of orpedsms Present within it. Such changes Inay be undesirable and intetw with wateuses." Sndth et al. (l999) indicated tha eopation of waters is mainly caused by h… 相似文献
73.
G. M. E. Kamh 《Environmental Geology》2007,52(8):1539-1547
Al-hambra is an immense and valuable archaeological site in Spain built on Sabika hill with red brick and natural sandy limestone.
It exhibits weathering features indicating salt weathering process. The main aim of this study is to examine weathering processes
and intensity acting on Al-hambra. Rock petrography and mineralogical composition have been examined using thin sections,
scanning electron microscope, X-ray diffraction and X-ray fluorescence; limits of rock’s physical parameters using ultrasonic
waves and mercury porosimeter; rock salt content through hydrochemical analysis. Salts attacking this structure are mainly
from wet deposition of air pollutants on the long term chemical alteration of rock’s carbonate content to its equivalent salts.
The salts’ concentration limit within the examined rock samples is considerably low but it is effective on the long run through
hydration of sulphate salts and/or crystallization of chloride salts. Rock texture type and its silica as well as clay content
reduces its resistance to internal stresses by salts as well as wetting and drying cycles at such humid area. The recession
in limits of physical parameters examined for deep seated and weathered limestone samples quantitatively reflects weathering
intensity on Al-hambra. 相似文献
74.
In a recent paper, Nof et al. (J Paleolimnol 35:417–439, 2006) suggest a physical mechanism which could account for the formation
of ice on Lake Kinneret (Sea of Galilee) in northern Israel. Based on the sea surface temperature record of sediment cores
from the Mediterranean Sea the authors argue that centennial-scale cold events had the potential to trigger local ‘springs
ice’ formation on the lake in the past. Here, we demonstrate that a closer inspection of the paleoceanographic record in combination
with correlation and regression analyses of meteorological data provides no evidence for such cold events in the lake region
during the last 10,000 years. Thus, the formation of ‘springs ice’ on Lake Kinneret was unlikely at least since the beginning
of the Neolithic. 相似文献
75.
陶器资源——江西红土岩开发 总被引:4,自引:0,他引:4
依据江西红土岩物质组成特征及与宜兴紫砂土的相似性,对江西红土岩进行了较系统的陶器实验与研究。江西红土岩系的化学成分、矿物成分及工艺特征适合陶器要求。按其分布规律和物质组成特征可分成两类:酸性红土岩和碱性红土岩。在详细分析两类岩系工艺性质的基础上,对江西红土岩这一陶器资源进行了产品开发。 相似文献
76.
77.
Giovanni Muttoni Dennis V. Kent James E.T. Channell 《Earth and Planetary Science Letters》1996,140(1-4):97-112
A new early Late Triassic paleopole for Adria has been obtained from the Val Sabbia Sandstone in the Southern Alps. As Early Permian and Jurassic-Cretaceous paleomagnetic data from para-autochthonous regions of Adria such as the Southern Alps are consistent with ‘African’ APWPs[1–2], paleomagnetic data from this region can be used to bolster the West Gondwana APWP in the poorly known Late Permian-Triassic time interval. The Southern Alpine paleopoles are integrated with the West Gondwana and Laurussia APWPs of Van der Voo [1] and used to generate a tectonic model for the evolution of Pangea. The Early Permian overall mean paleopole for West Gondwana and Adria, in conjunction with the coeval Laurussia paleopole, support Pangea B of Morel and Irving [3]. The Late Permian/Early Triassic and the Middle/Late Triassic paleopoles from Adria and Laurussia support Pangea A-2 of Van der Voo and French [4]. The phase of transcurrent motion between Laurasia and Gondwana[5] that caused the Pangea B to A-2 transition occurred essentially in the Permian (at the end of Variscan orogeny) with an average relative velocity of approximately 10 cm/yr. Finally, the Late Triassic/Early Jurassic paleopoles from West Gondwana and Laurussia agree with Pangea A-1 of Bullard et al. [6], the widely accepted Pangea configuration at the time of the Jurassic breakup. 相似文献
78.
青藏高原东北部古喀斯特过程与环境 总被引:6,自引:0,他引:6
本文介绍了青藏高原东北部地区的古喀斯特现象,并对相关沉积进行了化学成、粘土矿物的X-射线衍射以及石英砂表面结构等气候代用指标的分析。分析结果一致,指示了温暖湿润的亚热带气候条件。重结晶方解石的裂变径迹测年结果表明,该地区古喀斯特发育于中中新世。 相似文献
79.
红层(盆)内外存在着工业金矿化现象,与红层(盆)有关的金矿化包括:次火山岩型、卡林型、穆龙套型、不整合脉型、风化壳型、热泉型以及砂金等众多类型。它们的形成过程及分布与红层(盆)关系密切。本文总结了与红层(盆)有关金矿化的成矿模式及找矿方向。 相似文献
80.
Summary The Delivery Tunnel South forms part of a system of tunnels for conveying water from Lesotho to South Africa. The tunnel was excavated primarily by tunnel boring machine in the sandstones of the Clarens Formation. These sandstones are uniformly graded and fine grained with quartz being the most abundant mineral. They are mostly of aeolian origin. Their unconfined compressive strength varies appreciably, from moderately strong to extremely strong. The boreability of the sandstones was investigated by the Norwegian Institute of Technology tests and the total hardness. These tests showed that these sandstones would be relatively easy to bore, although moderately abrasive. The prediction proved correct. In fact, excavation of the tunnel was completed 20 months ahead of schedule, the rock conditions being better than expected. The long-term durability of these sandstones was investigated to establish criteria for concrete lining of the tunnel. A series of tests were undertaken to evaluate the durability. These included a number of soaking tests using different fluid media, wet and dry testing, erosion tests and brushing tests. This testing programme suggested that concrete lining of the intact sandstone was probably only required where the strength of the sandstone was less than 20 MPa and that therefore only a small percentage of the tunnel need be lined. 相似文献