THE NORTHWARD PROPAGATION OF THE ARC TECTONICS OF THE NORTHEAST PAMIR AND NORTHWEST TARIM BASIN     

Li Yingzhen  Shen Jun 《地学前缘》2000,(Z1)

THE NORTHWARD PROPAGATION OF THE ARC TECTONICS OF THE NORTHEAST PAMIR AND NORTHWEST TARIM BASINThisworkispartoftheresearchproject“themechanismofJiashistrongearthquakeswarmandprediction ofearthquakeriskinthenortheastPamir  相似文献   

STUDY ON THE BASIC IGNEOUS EVENT IN CENTRAL QIANGTANG, TIBET     

Li Cai  Yang Deming  Wang Tianwu  Yang Rihong  Liu ShenWT  ”BX 《地学前缘》2000,(Z1)

STUDY ON THE BASIC IGNEOUS EVENT IN CENTRAL QIANGTANG, TIBET  相似文献   

Extraction of plasmid-like DNA and high-quality total DNA from Porphyra yezoensis   总被引：3，自引：0，他引：3  

Guo Baotai  Dai Jixun  Shen Songdong  Bi Yuping  Shan Lei  Li Guangcun 《海洋学报(英文版)》2000,19(2):83-88

I~ODWrIONExtraction of DNA from Porphyra po~nsis is very difficult due tO its high content ofpolysaccharides. TO avoid the interference Of POlysaccharides, HOng et al. (1992) used LiCI tosoften Porphyra thalli cells to release DNA directly without lysing the thalli, hoWever, the procedure is problematic in the isolation of high-quality DNA. Kitade et al. (1996) established a complicated procedure which includes the grindiflg of material in liquid nitrogen, lysing of material inextra…  相似文献   

南四湖底泥污染及其变化过程     

张祖陆  孙娟  王琳  Shen Ji 《地理学报(英文版)》2004,14(1):121-125

In order to research the changing process of the pollution from the formation of Nansihu Lake, this study determined the isotope age and depositional rate and analyzed the organic geo-chemical quotas and heavy metal quotas of two sedimentary profiles of Weishan and Dushan lakes. Research results showed that from the formation of Nansihu Lake, the change of the pollution could be divided into four phrases. At the early phrase of the formation, the organic matters of the lake mainly derived from the exotic matters and had a close relation to the effect on the water and sands from the Huanghe (Yellow) River. At the middle and late phrases of the development, the endogenous matters of the lake became the main and stable source of the organic matters. The overflow of the Huanghe River, the excavation of the Grand Canal and the cut of trees caused the changes of the historic pollution. In recent 20 years, the modem industrial pollution from the organic matters and heavy metals has an increasingly heavy tendency.  相似文献   

Background Seismicity and Its Application to Seismic Hazard Assessment in the North China Region     

Wang Hui  Cao Jianling  Shen Xuhui 《中国地震研究》2011,25(4):395-408

The historical earthquake activity is intense in the North China region. However, no middle-sized earthquakes have occurred in the last decades in the region since the MS6.2 earthquake in the Zhangbei region in 1998. The quiescence of moderate and strong earthquakes is quite prominent in North China. In this paper, we use small earthquake records in 1970~2009 to study background seismic activity in the North China region. The spatial distributions of seismic parameters are presented, including b-value, the maximum magnitude and annual occurrence probability of earthquakes of M≥6.0. Our results show regions with low b-value that include the Yuncheng region in the Shanxi rift, the Suqian region located in the Tancheng-Lujiang fault zone and the Shijiazhuang region in the Taihangshan block. Our analysis on the synthetic spatial pattern of seismicity indicate that seismicity in the North China region is mainly affected by the regional dynamic factors of deep structures.  相似文献   

Will Glacier No.1 Tianshan exist in the 22nd century?     

WenYing Wang  YongPing Shen 《寒旱区科学》2011,3(3):0206-0215

Mountains have been described as the water towers of the world. Almost all major rivers have their sources in mountains; glaciers are important water resources that contribute meltwater to river discharge. Glaciers participate in the global water cycle and, with their solid water storage, are an important component of the water balance. As solid reservoirs, glaciers continue to receive the mass nourishment of solid precipitation from the atmosphere, and their meltwater feed and regulate river discharge. Physical changes in glaciers are an indicator of climate change. Over the past half century, the global temperature has increased by 1–2 °C, which emphasizes the urgent task of monitoring glaciers and predicting their trend. As an example, we have investigated, researched, and surveyed Glacier No.1 in the Urumqi River source, Tianshan (abbr. Glacier No.1 Tianshan or Glacier No.1) for half a century. We have found an increase by degrees of the glacial regression during the last 400 years and discovered a terminal moraine which is forming today. The global temperature is rising continually, while the local glacial temperature is 0.4 times that of the global temperature change. Thus, we forecast that Glacier No.1 Tianshan will disappear during the late 21^st Century (2074–2100 A.D.).  相似文献   

GPS DATA INVERSION OF KINEMATIC MODEL OF MAIN FAULTS IN YUNNAN     

Shen Chongyang  Wu Yun  Wang Qi  You Xinzhao  Qiao Xuejun 《大地测量与地球动力学》2003,23(Z1)

1　IntroductionThemodernspacegeodesytechnology (GPSes pecially)israpidlydeveloping ,andisabletoprecise lymonitorongoingsurfacechangeprocessatun precedentedspatialandtemporalresolution .Soithasgraduallybecomethemostsuitabletooltoob servegeodynamicalphenomena[1 - 5] .Theearthquakepreparationandoccurrencearecloselyrelatedtofaultanditsmovement.Activefaultanditsquantitativeanalysisisstillthepredomi nantfieldofseismologicalresearch[6,7] .Faultdislo cationmaycausecrustaldeformationaroundit.Onthebas…  相似文献   

G328: A Small-Amplitude Red Variable with a Period Near One Day     

Bao-An Yao  Chang-Jun Shen  Chun-Sheng Zhang  Han-Ming Hu  Qing Lin Shanghai Astronomical Observatory  Chinese Academy of Sciences  Shanghai Purple Mountain Observatory  Chinese Academy of Sciences  Nanjing National Astronomical Observatories / Yunnan Observatory  Chinese Academy of Sciences  Kunming 《中国天文和天体物理学报》2006,6(5)

G328 = A65 = L3314 (V = 13.83, B-V = 1.91) is a field star in the direction of the globular cluster M4. If we take E(B - V) = 0.40, then its (B - V)0 = 1.51, corresponding to a spectral type of K5III if it is a giant star; or of dM2 if it is a dwarf. Observations at both the MSSSO and Yunnan Observatory have shown that G328 is a new variable with peak to peak amplitude - 0.05 mag in V. While it is not unusual for so red a star to be a variable, special attention must be paid to its short period of about one day. If the variability is due to pulsation, the spectral type and luminosity as well as effective temperature should be determined in order to compare it with Xiong's theory.  相似文献   

Global Axisymmetric Stability Analysis for a Composite System of Two Gravitationally Coupled Scale-Free Discs     

Yue Shen  Yu-Qing Lou Department of Physics & Center for Astrophysics  Tsinghua University  Beijing  National Astronomical Observatories  Chinese Academy of Sciences  Beijing Department of Astronomy  Astrophysics  The University of Chicago  South Ellis Avenue  Chicago  IL USA   《中国天文和天体物理学报》2004,4(6):541-552

For a composite system of gravitationally coupled stellar and gaseous discs, we have carried out a linear stability analysis for axisymmetric coplanar perturbations using the two-fluid formalism. The background stellar and gaseous discs are taken to be scale-free with all physical variables varying as powers of the cylindrical radius r with compatible exponents. The unstable modes set in as neutral modes or stationary perturbation configurations with angular frequency ω=0. The axisymmetric stable range is bounded by two marginal stability curves derived from stationary perturbation configurations. Because of the gravitational coupling between the stellar and the gaseous discs, one only needs to consider the parameter regime of the stellar disc. There exist two unstable regimes in general: a collapse regime corresponding to large-scale perturbations and a ring-fragmentation regime corresponding to short-wavelength perturbations. The composite system will collapse if it rotates too slowly and will succumb to ring-fragmentation instabilities if it rotates sufficiently fast. The overall stable range against axisymmetric perturbations is determined by a necossary D-criterion involving the effective Mach number squared Ds^2 (the squared ratio of the stellar disc rotation speed to the stellar velocity dispersion up to a numerical factor). Different mass ratio δ and sound speed ratio of the gaseous and stellar disc components will alter the overall stability. For spiral galaxies or circumnuclear discs, we further include the dynamical effect of a massive dark matter halo. Astrophysical applications to disc galaxies, proto-stellar discs and circumnuclear discs are given as examples.  相似文献   

Zircon U-Pb Age,Geochemical, and Sr-Nd-Pb-Hf Isotopic Constraints on the Time Frame and Origin of Early Cretaceous Mafic Dykes in the Wuling Mountain Gravity Lineament,South China     

CHEN Xiaoqing  LIU Shen  FENG Caixi  XU Jingyan  ZHAO Huibo  FENG Guangying  Ian M. COULSON  SUN Jinggui  FAN Yan 《《地质学报》英文版》2021,95(2):419-438

In view of the importance of mafic dyke swarms and their contribution to current scientific problems relating to South China, herein, we present the findings of studies on twenty–five representative mafic dykes cropping out in Hunan Province and Guangxi Zhuang Autonomous Region, within the southern Wuling Mountain gravity lineament, China. These results include new zircon LA-ICP-MS U-Pb age, whole rock geochemical, Sr-Nd-Pb isotopic, and zircon Hf isotopic data for these dykes. The dykes formed between 131.5 ± 1.2 and 121.6 ± 1.1 Ma, and have typical doleritic textures. They fall into the alkaline and shoshonitic series, are enriched in light rare earth elements(LREE), some large ion lithophile elements(LILE; e.g., Rb, Ba, and Sr), Th, U, and Pb, and are depleted in Nb, Ta, Hf, and Ti. Moreover, the dolerites have high initial87 Sr/86 Sr ratios(0.7055–0.7057), negative εNd(t) and zircon εHf(t) values(-14.8 to-11.9,-30.4 to-14.9), and relatively constant initial Pb isotopic ratios(that are EM1-like, 16.77–16.94, 15.43–15.47, and 36.84–36.92 for 206 Pb/204 Pb,207 Pb/204 Pb, and 208 Pb/204 Pb, respectively). These results indicate that the dykes were likely derived from magma generated through low-degree partial melting(1.0%–10%) of an EM1-like garnet–lherzolite mantle source. The parental magmas fractionated olivine, clinopyroxene, plagioclase, and Ti-bearing phases with negligible crustal contamination, during ascent and dyke emplacement. Several possible models have been proposed to explain the origin of Mesozoic magmatism along the Wuling Mountain gravity lineament. Herein we propose a reasonable model for the origin of these mafic dykes,involving the collision between the paleo-Pacific Plate and South China, which led to subsequent lithospheric extension and asthenosphere upwelling, resulting in partial melting the underlying mantle lithosphere in the Early Cretaceous, to form the parental magmas to the WMGL mafic dykes, as studied.  相似文献