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Synergetic-bifurcated prediction model of slope occurrence and its application

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Science China(Technological Sciences) 2003年第Z1期46卷 69-77页

作者： HUANG Zhiquan & WANG Sijing North China institute of Water Conservancy and Hydroelectric Power, Zhengzhou 450008, China institute of {2. & geophysics, Chinese Academy of Sciences, beijing 10002., China N China Inst Water Conservancy & Hydroelect Power Zhengzhou 450008 Peoples R China Chinese Acad Sci Inst Geol & Geophys Beijing 100029 Peoples R China

Landslide prediction is one of the most important aspects of prevention and control for geological hazards and the environmental protection. In order to study the nonlinear methods for landslide prediction, the synergetic-bifurcated model of predicting the timing of slope failure is established by combining Synergetics with Bifurcation Theory based on single-state variable friction law in this paper. The synergetic effects and bifurcated process of the factors in the slope evolution can be characterized in the model. Taking the Xintan Landslide as an example, the prediction of landslide is carried out based on the model suggested.

关键词： friction law, landslide, synergetic-bifurcated model, time prediction.

The Yanshanian Orogeny and Two Kinds of Yanshanides in Eastern-Central China

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Acta Geologica Sinica(English Edition) 2005年第4期79卷 507-518页

作者： wu genyao institute of geology and {2. Chinese Academy of Sciences Beijing 100029

The Tan-Lu Fault was once a transform fault in the Paleotethys, west of which was the Qinling-Dabie Ocean separating the Yangtze Craton from the North China Craton, and east of which was the Su-Lu Ocean separating the Su-Wan Block from the Jiao-Liao Craton. The Qinling-Dabie Ocean closed in the Indosinian orogeny, which created the China-Southeast Asia Subcontinent, with the Tan-Lu Fault becoming a marginal shear zone along the newly-formed amalgamated subcontinent. The Su-Lu Ocean subducted partly in the ***, but not closed. In the Jurassic and Early Cretaceous, the Su-Wan Block drifted northwards with subduction of the Su-Lu Ocean and moved westwards to converge the subcontinent by sinistral sheafing of the ENE-striking fractures. The Su-Lu Ocean finally closed and the Su-Wan Block collided with the Jiao-Liao Craton in the Early Cretaceous, which constituted a part of the magnificent interplate Yanshanides. The interplate orogeny rejuvenated the fossil sutures and deep fractures, as well as the Indosinian orogen, and the intraplate （intracontinental） Yanshanian orogeny occurred in the subcontinent. The East Asia Yanshanides, consisting of the interplate orogens in the outer side and the intraplate orogens in the inner side, collapsed quickly in the latest Early Cretaceous and Late Cretaceous. The eastern China area entered a tensile period from the Eogene, and the tectonic differentiation between the central and eastern China areas since the Jurassic was further strengthened.

关键词： Yanshanian orogeny interplate orogen intraplate (intracontinental) orogen East Asia Yanshanides eastern-central China

APPLICATIONS OF ORTHOGONALITY THEORY OF DISCRETE NORMAL MODES TO THE IDENTIFICATION OF FREE OSCILLATION EIGENFREQUENCIES AND DETERMINA TIONS OF SPECTRAL PEAK POSITIONS AND SPECTRAL LINE WIDTHS

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中国科学B辑(英文版) 1985年第6期28卷 641-654页

作者：吴文京 institute of geophysics State Seismological Bureau beijing

Owing to the loss of the orthogonality relations of discrete normal modes of free oscillations of the Earth in practical analysis, not only stacking method fails to give the desired results, but also stripping method may lead to large errors and even mis-identifications for certain normal modes. For this reason, a method in which the data from many earthquakes are used and appropriately weighted in order to make the orthogonality relations of discrete normal modes approximately satisfied is put forward. In addition, the conditions under which the orthogonality relations of discrete normal modes hold exactly within the range of a given degree and order have been found.

关键词： desired stripping exactly stacking latitude coordinates identifying 二尹 assumed satisfy

FORMATION AND EUOLUTION OF TETHYS IN THE TIBETAN PLATEAU

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地学前缘 2000年第S1期7卷 334-335页

作者： Pan Yusheng[WT5,5”BX](institute of geology and {2., Chinese Academy of Sciences, beijing 10002.,China)

The formation of the Tibetan Plateau is closely related to the evolution of Tethys. There have been many researchers and articles concerning the Tethys since *** proposed the concept in 1893. It means a large ocean which lies between Eurasia and Gondwanaland. With the development of Tethyan research, some new terms, appeared such as Neo\|Tethys, Paleo\|Tethys, and Proto\|Tethys, representing the Tethys in Mesozoic—Cenozoic, late Paleozoic and early Paleozoic respectively. The trace of an ocean from Sinian to Ordovician was discovered during the scientific expedition and Proto\|Tethys was proposed to name the ocean. Therefore, the Tibetan Plateau is the main scope of the Eastern Tethys. It can be divided c losely related into three zones which represent the main oceanic locations in th ree different *** Northern Tethyan Region lies in the Kunlun and Qilian Mountains, its remnant is the Fifth Suture Zone. It is also the northern boundary of the Tibetan Plateau The rift initiated after the continental basement had been formed in Sinian and gradually developed into an ocean, which was named Proto\|Tethys, the earliest Tethyan ocean known up to now. The petrochemical compositions of pillow lava in this zone show the characteristics of mid\|ocean ridge tholeiite basalt and the pelagic ophiolitic flysch were well developed, indicating a matured ocean. It was closed in Ordovician and Silurian.

关键词： formation and evolution Tethys Tibetan plateau suture zone structural deformation Gondwana land

TAKE ANOTHER VISION TO THE UPLIFT OF THE QING—ZANG (TIBETAN) PLATEAU BASED ON CENOZOIC VOLCANISM

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地学前缘 2000年第S1期7卷 370-371页

作者： Liu Jiaqi [WT5,5”BX](institute of geology and {2.,Chinese Academy of Sciences,beijing 10002., China)

The emergence of the Qing—Zang plateau is among the most important geological events on the globe since the Cenozoic Era. Many geological issues can find answer from here. The major issues concerning plateau probably have three: (1) geodynamics, timing and speed of the plateau uplift;(2. The plateau uplift impact on surrounding environment;(3) mineral resources in the plateau. The authors want to focuses on first issue based on volcanisms occurred in interior and surrounding of the plateau, The new opinions are following:(1) Each volcanic eruptive episode corresponded to strong uplift stage;(2. The dynamic mechanism of the plateau uplift can not ignore another force from west beyond collision between Indian and Eurasia plates from South;(3) The surrounding volcanic chain is not only related to the collision from South, but also from west.

关键词： Tibetan plateau the Cenozoic volcanism volcanic chain surro unding plateau west collision uplift mechanism

Low-temperature magnetic properties of horse spleen ferritin

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Chinese Science Bulletin 2010年第27期55卷 3174-3180页

作者： TIAN LanXiang 1,2.CAO ChangQian 1,2.LIU QingSong 1,2.&PAN YongXin 1,2.1Key Laboratory of the Earth’s Deep Interior,institute of geology and {2.,Chinese Academy of Sciences,beijing 10002.,China 2.ranco-Chinese Biomineralization and Nano-structures Laboratory,beijing 10002.,China Key Laboratory of the Earth’s Deep Interior Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China Franco-Chinese Biomineralization and Nano-structures Laboratory Beijing China

The magnetic properties of the antiferromagnetic cores in ferritin are of importance in the construction and improvement of ferritin-based magnetic resonance imaging systems and their application to environmental *** this study,we carry out integrated magnetic and transmission electron microscopy analyses of horse spleen ferritin(HoSF)to understand the relationships between the magnetic behavior of HoSF and temperature,applied field and grain-size *** R-value from the Wohlfarth-Cisowski test for the investigated sample at 5 K was 0.46,indicating very weak magnetostatic interactions among the nanoparticles of *** nanoparticles of HoSF show superparamagnetic properties at room temperature,while below the blocking temperature of Tb≈12.K it has a net magnetic moment that comes from the uncompensated spins of the nanoparticle surface or *** thermal relaxation process of HoSF follows the Néel-Arrhenius *** low-temperature AC susceptibility data,we calculated the effective magnetic anisotropy energy Ea=(5.52.0.16)×10-2. J;the effective magnetic anisotropy energy constant Keff=(4.65±0.14)×10 4 J/m3 and the pre-exponential frequency factor f0 =(4.52.2.93)×1011 *** values are useful in understanding the magnetic behavior of the antiferromagnetic nanoparticles and their potential application in biomedical technology.

关键词：马脾铁蛋白低温度磁性质透射电子显微镜磁各向异性常数纳米粒子生物医学技术交流磁化率

Dating of the Karakorum Strike-slip Fault

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Acta Geologica Sinica(English Edition) 2001年第1期75卷 10-18页

作者： ZHOU Yong, XU Ronghua, YAN Yuehua, PAN Yusheng,Tsanyao Frank YANG, Wei LO and wu Chunming Laboratory of Lithosphere Tectonic Evolution, institute of {2. and {2., Chinese Academy of Sciences, beijing 10002.Department of {2., National Taiwan University, 2.5 Choushan Road, Taipei 106-17, TaiwanDepartment of {2., Chinese Culture University, Hwa-kang, Yang-Ming-Shan, Taipei, Taiwan institute of {2., Chinese Academy of Geological Sciences, beijing 100037 Chinese Acad Sci Inst Geol & Geophys Lab Lithosphere Tecton Evaluat Beijing 100029 Peoples R China Natl Taiwan Univ Dept Geol Taipei 10617 Taiwan Chinese Culture Univ Dept Geol Taipei Taiwan Chinese Acad Geol Sci Inst Geol Beijing 100037 Peoples R China

This paper mainly discusses the timing of the Karakorum strike-slip fault, and gives a brief introduction of its structures, offset, and deformational style. This fault strikes NNW-SSE. Asymmetrical folds, stretching lineation, S-C fabrics, feldspar and quartz s?-porphyroclasts, domino structure, shear cleavages and faults in the fault zone are products of tectonic movements. They all indicate a dextral slip sense of faulting. Mylonitic bands are widely developed along this fault. Phengite appears, indicating rather high deformational pressure. Geochronological data indicate that the Karakorum strike-slip faulting occurred from 6.88±0.36 to 8.75±0.2. Ma. The cumulative displacement from Muztag Ata to Muji is about 135 km.

关键词： Karakorum fault kinematics timing displacement

Cold Thermal Anomalous Structure within Lower Mantle and Its Geodynamic Implications

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Journal of China University of Geosciences 2001年第2期12卷 160-164页

作者： Xiong Xiong institute of Geodesy and geophysics, Chinese Academy of Sciences, {2.han 430077 institute of geology and geophysics, Chinese Academy of Sciences, beijing 100101 Hsu Houtze institute of Geodesy and geophysics, Chinese Academy of Sciences institute of Geodesy and geophysics Chinese Academy of Sciences institute of geology and {2. Chinese Academy of Sciences

The lateral temperature anomalous structure of the lower mantle is reconstructed from the seismic tomographical model and high temperature and high pressure laboratory results. A significant correlation between the distribution of the cold anomaly and the location of past subduction belts shows that the shallower anomaly corresponds to the younger subduction sites, while the deeper anomaly to the older ones. This correlation also suggests that the cold anomaly may have come from the subduction slabs and the scale of mantle convection may have been completed. The coldest and largest anomaly is concentrated near the core mantle boundary (CMB). Few cold anomalies float in the shallower and middle parts of the lower mantle, suggesting that the downward migration of the subduction slabs, discontinuous and step like, may be divided into the following three stages: subduction, stagnation at the 670 km discontinuity due to the phase transition, and disintegration when the size exceeds the critical point.

关键词： lower mantle cold thermal anomaly geodynamic implication.

^(40)Ar-^(39)Ar thermochronology of two ductile shear zones from Yiwulüshan,West Liaoning Region: Age constraints on the Mesozoic tectonic events

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Chinese Science Bulletin 2002年第13期47卷 1113-1118页

作者： ZHANG Xiaohui, LI Tiesheng & PU ZhipingResearch Center of Mineral Resources Exploration, institute of geology and {2., Chinese Academy of Sciences, beijing 100101, China Guangzhou institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 51 Research Center of Mineral Resources Exploration Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China Guangzhou institute of Geochemistry Chinese Academy of Sciences Guangzhou China

Two ductile shear zones trending EW and NNE respectively not only controlled the tectonic framework of the northern North China, but also constrained the geody-namic background for gold mineralization in this region. Field observations and microstructural analyses reveal that the EW trending ductile shear zones are mainly contributed to dextral compressional deformation resulting from top-to-the-southeast oblique thrust shearing, whereas the NNE trending ones are genetically related to sinistral strike-slip and extensional faulting. One sample from the former yielded an 40Ar-39Ar plateau age of (2.9±4) Ma (Bi) and two samples from the latter gave 40Ar-39Ar plateau ages of (116± 2. Ma (Bi) and (12.±3) Ma (Bi). These ages provide constraints on the top-to-the-southeast oblique thrusting event occurring in Late Triassic and the sinistral extensional and strike-slip faulting event which occurred in Early Cretaceous.

关键词： 40Ar-39Ar age biotite ductile shear zone West Liaoning Region.