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121.
Dong YunPeng Zhang GuoWei Zhou DingWu Luo JinHai Zhang ChengLi Xia LinQi Xu XueYi Li XiangMin 《中国科学D辑(英文版)》2007,50(1):17-24
The properties and tectonic significance of the fault bound zone on the northern margin of the Central Tianshan belt are key
issues to understand the tectonic framework and evolutionary history of the Tianshan Orogenic Belt. Based on the geological
and geochemical studies in the Tianshan orogenic belt, it is suggested that the ophiolitic slices found in the Bingdaban area
represent the remaining oceanic crust of the Early Paleozoic ocean between the Hazakstan and Zhungaer blocks. Mainly composed
of basalts, gabbros and diabases, the ophiolites were overthrust onto the boundary fault between the Northern Tianshan and
Central Tianshan belts. The major element geochemistry is characterized by high TiO2 (1.50%–2.25%) and MgO (6.64%–9.35%), low K2O (0.06%–0.41%) and P2O5 (0.1%–0.2%), and Na2O>K2O as well. Low ΣREE and depletion in LREE indicate that the original magma was derived from a depleted mantle source. Compared
with a primitive mantle, the geochemistry of the basalts from the Bingdaban area is featureded by depletion in Th, U, Nb,
La, Ce and Pr, and unfractionated in HFS elements. The ratios of Zr/Nb, Nb/La, Hf/Ta, Th/Yb and Hf/Th are similar to those
of the typical N-MORB. It can be interpreted that the basalts in the Bingdaban area were derived from a depleted mantle source,
and formed in a matured mid-oceanic ridge setting during the matured evolutionary stage of the Northern Tianshan ocean. In
comparison with the basalts, the diabases from the Bingdaban area show higher contents of Al2O3, ΣREE and HFS elements as well as unfractionated incompatible elements except Cs, Rb and Ba, and about 10 times the values
of the primitive mantle. Thus, the diabases are thought to be derived from a primitive mantle and similar to the typical E-MORB.
The diabases also have slight Nb depletion accompanying no apparent Th enrichment compared with N-MORB. From studies of the
regional geology and all above evidence, it can be suggested that the diabases from the Bingdaban area were formed in the
mid-oceanic ridge of the Northern Tianshan ocean during the initial spreading stage.
Supported by the Major State Research Program of PRC (Grant No. 2001CB409801), the National Natural Science Foundation of
China (Grant Nos. 40472115 and 40234041) and the State Research Program of China Geological Survey (Grant No. 2001130000-22) 相似文献
122.
Authors of the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) received guidance on reporting
understanding, certainty and/or confidence in findings using a common language, to better communicate with decision makers.
However, a review of the IPCC conducted by the InterAcademy Council (2010) found that “the guidance was not consistently followed in AR4, leading to unnecessary errors . . . the guidance was often
applied to statements that are so vague they cannot be falsified. In these cases the impression was often left, quite incorrectly,
that a substantive finding was being presented.” Our comprehensive and quantitative analysis of findings and associated uncertainty
in the AR4 supports the IAC findings and suggests opportunities for improvement in future assessments. 相似文献
123.
The empirical rainfall threshold concept and the physical-based model are two commonly used approaches for the assessment
of shallow landslides triggered by rainfall. To investigate in detail the rainfall-triggered shallow landslides, many physical-based
models coupling the infinite slope stability analysis with the rainfall infiltration modeling in variably saturated soil were
developed. However, in those physical-based shallow landslide models, the unit weight and the unsaturated shear strength were
assumed constant rather than depending on the degree of saturation. In this study, the effects of the unit weight and the
unsaturated shear strength as function of degree of saturation on rainfall-triggered shallow landslides are examined. Several
designed scenarios and a real case scenario are used to conduct the examinations. The results show that not only the occurrence
of shallow landslides but also the failure depth and the time to failure could be misassessed if the influences of degree
of saturation on the unit weight and the unsaturated shear strength are neglected. 相似文献
124.
This paper is presenting the results from near-surface geophysical surveys near the waste site of Hoc Mon in southern Vietnam
where leachate contamination has been recognized at the surface. Using EM and GPR surveys, we were able to determine the lateral
extent of a contaminated area of high electrical conductivity and have identified channels that concentrate the contaminant
flow. The simple relationship between the electrical resistivity and the leachate concentration is suggested and estimated
the in situ leachate concentration from the inversion of the EM data; values are as high as 40%. Thanks to a permeability barrier leachate
flow is confined to the shallow subsurface, making it easier to apply possible site remediation projects. 相似文献
125.
Effects of rapidly changing ionospheric weather are critical in high accuracy positioning, navigation, and communication applications. A system used to construct the global total electron content (TEC) distribution for monitoring the ionospheric weather in near-real time is needed in the modern society. Here we build the TEC map named Taiwan Ionosphere Group for Education and Research (TIGER) Global Ionospheric Map (GIM) from observations of ground-based GNSS receivers and space-based FORMOSAT-3/COSMIC (F3/C) GPS radio occultation observations using the spherical harmonic expansion and Kalman filter update formula. The TIGER GIM (TGIM) will be published in near-real time of 4-h delay with a spatial resolution of 2.5° in latitude and 5° in longitude and a high temporal resolution of every 5 min. The F3/C TEC results in an improvement on the GIM of about 15.5%, especially over the ocean areas. The TGIM highly correlates with the GIMs published by other international organizations. Therefore, the routinely published TGIM in near-real time is not only for communication, positioning, and navigation applications but also for monitoring and scientific study of ionospheric weathers, such as magnetic storms and seismo-ionospheric anomalies. 相似文献
126.
Chen Qiu 《中国海洋湖沼学报》1986,4(4):372-378
Acetes chinensis always ovulate in the dark at night. Two to five hours before ovulation, the mature oocytes change from white
to orange. In the meantime, meiosis of the oocytes occurs, and reaches the metaphase just prior to ovulation. If ovarian colour
change starts in the dark at night but ovulation does not start by break of dawn, ovulation will be inhibited and meiosis
of the cells will be blocked. 相似文献
127.
Enrique Pérez Richard de Grijs Rosa M. González Delgado 《Astrophysics and Space Science》2009,324(2-4):79-81
128.
129.
吉黑东部金矿床集中分布于小兴安岭北麓、完达山和太平岭(东宁-延边),矿床类型以斑岩型-浅成低温热液型矿床为主。成矿年代大约为110 Ma左右。稳定同位素显示成矿流体具有岩浆水特征,而成矿物质则主要来源于深源岩浆,这说明吉黑东部金成矿可能与岩浆活动有关。同时,研究显示吉黑东部广泛发育一套120~95 Ma的中酸性火山-侵入岩,其与110 Ma金成矿事件时空关系密切。这套火山-侵入岩在矿区表现为英安-流纹质或安山-英安质火山岩组合和闪长玢岩、花岗斑岩及花岗岩等脉岩和小侵入体。而岩石化学特征则表明其属中酸性的钙碱性系列,为一套俯冲流体交代地幔楔起源的岩浆。区域对比研究表明,吉黑东部金成矿与俄罗斯远东地区Sikhote-Alin锡成矿、韩国南部金-银成矿可能处于同一大地构造环境的不同构造部位。成矿年代从吉黑东部向东南方向有变年轻的趋势,且成矿岩浆岩的酸性成分增强而幔源成分减少。综合区域岩浆岩和区域成矿特征,表明吉黑东部存在一期110 Ma的金成矿事件,其与中生代晚期板块俯冲及其后的岩石圈拆沉作用和弧后伸展有关,成矿大地构造环境为大陆边缘弧。 相似文献
130.
Hong Lu Tengshui Chen Kliti Grice Paul Greenwood Ping’an Peng Guoying Sheng 《Organic Geochemistry》2009,40(8):902-911
An unusual series of C22–C27 monounsaturated sterenes and C24–C30 tetracyclic terpanes (17,21-secohopanes) were detected in relatively high concentrations in an immature evaporitic marl sediment of the Jinxian Sag, Bohai Bay Basin, North China. The site of unsaturation in these novel sterenes is assigned tentatively to the D ring on the basis of mass spectral interpretation, which also distinguishes them from reported unsaturated sterenes. Other hydrocarbon biomarker or stable isotope characteristics are indicative of microbial (e.g. methyl hopanes), phytoplankton or higher plant (depleted δ13C values of isoprenoids and hopanes) inputs and an anoxic carbonate depositional environment (hexacyclic hopanes; tetracyclic terpanes). The hydrocarbon composition showed no obvious biodegradation and the relatively high concentration of unsaturated terpenoids (e.g. gammacerene) and low values of other established maturity parameters (Ts/Tm = 0.23; Ro = 0.44%; Tmax = 417 °C), are consistent with sediments of low maturity. The novel, low molecular weight sterenes and the tetracyclic terpanes may be early diagenetic products of microbial sources in a carbonate environment. 相似文献