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1.
The hydrogen isotopic composition(δD) of n-alkanes in lacustrine sediments is widely used in palaeoenvironmental studies, but the heterogeneous origins and relative contributions of these lipids provide challenges for the interpretation of the increasing dataset as an environment and climatic proxy. We systematically investigated n-alkane δD values from 51 submerged plants(39 Potamogeton, 1 Myriophyllum, and 11 Ruppia), 13 algae(5 Chara, 3 Cladophora, and 5 Spirogyra) and 20 terrestrial plants(10 grasses and 10 shrubs) in and around 15 lakes on the Tibetan Plateau. Our results demonstrate that δD values of C_(29) nalkane are correlated significantly with the lake water δD values both for algae(R~2=0.85, p0.01, n=9) and submerged plants(R~2=0.90, p0.01, n=25), indicating that δD values of these algae and submerged plants reflect the δD variation of lake water. We find that apparent hydrogen isotope fractionation factors between individual n-alkanes and water(εa/w) are not constant among different algae and submerged plants, as well as in a single genus under different liminological conditions, indicating that the biosynthesis or environmental conditions(e.g. salinity) may affect their δD values. The δD values of submerged plant Ruppia in the Xiligou Lake(a closed lake) are significant enriched in D than those of terrestrial grasses around the lake(one-way ANOVA,p0.01), but the algae Chara in the Keluke Lake(an open lake) display similar δD values with grasses around the lake(one-way ANOVA, p=0.8260.05), suggesting that the n-alkane δD values of the algae and submerged plants record the signal of D enrichment in lake water relative to precipitation only in closed lakes in arid and semi-arid area. For each algae and submerged plant sample, we find uniformed δD values of different chain length n-alkanes, implying that, in combination with other proxies such as Paq and Average Chain Length, the offset between the δD values of different chain length n-alkanes can help determine the source of sedimentary n-alkanes as well as inferring the hydrological characteristics of an ancient lake basin(open vs closed lake). 相似文献
2.
正The International Conference for the Decade Memory of the Wenchuan Earthquake and the4th International Conference on Continental Earthquake will be held by China Earthquake Administration in Chengdu,Sichuan,China,on May 12-14,2018.On May 12,2008(Monday),at 14:08:04(Beijing time),an magnitude 8.0 earthquake 相似文献
3.
Zhang Guomin 《中国地震研究》2007,21(1):1-15
The paper describes firstly the principles and scientific train of thought involved in determining the significant seismic monitoring and protection regions (SSMPR) in China. The principles include the gradation principle, i.e. the national level SSMPR and the provincial level SSMPR, the principle of highlighting priorities, namely, the area of an SSMPR should be a fraction of the total area of the country or of the respective province, but the earthquake losses incurred in SSMPR should be a major proportion of the national or provincial ones. The scientific train of thought adopted is to determine the SSMPR on the basis of seismic hazard assessment and loss estimation. Secondly, it reviews the achievements in determining the SSMPRs for the period from 1996 to 2005. The result shows that 10 strong earthquakes occurred during that period in the areas with earthquake monitoring and prediction capability available on the Chinese continent, 8 of which occurred in SSMPRs with the economic loss and death toll accounting for 67% and 92% of the total loss on the Chinese mainland. Lastly, the paper introduces preparatory research for determining the SSMPR for the period from 2006 to 2020, including decade-scale mid-and long-range seismic risk assessment based on seismology, seismogeology, geodesy, earthquake engineering, sociology and stochastics and so on, and the national seismic risk probability map, the seismic hazard (intensity) map, earthquake disaster losses map and the comprehensive seismic risk index, etc. obtained for the period of 2006 to 2020. 相似文献
4.
（金延龙，赵卫明）ＡｎｉｍｐｒｏｖｅｍｅｎｔｏｎｔｈｅｍｅｔｈｏｄｏｆｔｈｅｐａｔｔｅｒｎｒｅｃｏｇｎｉｔｉｏｎＩＣＨＡＭａｎｄｉｔｓａｐｐｌｉｃａｔｉｏｎ￥Ｗｅｉ－ＭｉｎｇＺＨＡＯａｎｄＹａｎ－ＬｏｎｇＪＩＮ（ＳｅｉｓｍｏｌｏｇｉｃａｌＢｕｒｅａｕ... 相似文献
5.
Introduction Many observation facts, rock-rupture experimental results, and theoretical research achievements proved that the sudden changes in ground deformation are the most possible earthquake short-term precursors. The observed sudden changes in deformation that related to the earthquake preparation are here called the precursory. The sudden change is mainly characterized by the highly changing velocity and greatly accumulated deformation amplitude. The sudden change in ground deformation… 相似文献
6.
Establishment and analyses on the unified horizontal crustal velocity fields in the Chinese mainland 总被引：5，自引：0，他引：5
~~Establishment and analyses on the unified horizontal crustal velocity fields in the Chinese mainland@李延兴
@胡新康
@黄城
@朱文耀
@帅平
@胡小工
@张中伏~~State Key Basic Development and Program Project(G09980407). 相似文献
7.
Based on fracture mechanics,a large amount of practically observed data are analyzed in this paper,and it is disclosed that the earth resistivity stations around the epicenter of a strong event have shown seismically an anomalous earth resistivity suddenly changed sequence.The maximum sudden change in the sequence tends to shift backward with the increase of epicentral distance,while it shifts forward with the increase of the magnitude of the earthquake.Also,the maximum sudden change expands from the epicenter to the peripheral areas.The result of study has shown that the obviousness degree of the anomalies is related to the measuring direction.The lithological contrast around the stations also influences the time of the anomaly occurrence.The maximum sudden change of the sequence will be advanced while the rock resistance to pressure is not good.On the basis of these findings,the authors propose that it might be possible to predict the three key elements of forthcoming earthquakes by using the suddenly 相似文献
8.
Shao Huicheng 《中国地震研究》2007,21(2):189-195
The gestation and occurrence of strong earthquakes are closely related to fault activity, which is not only revealed by abundant experimentation and seismism but also proved by modern seismology. On the Chinese mainland, the relation between earthquake activity and active faults is one of the bases for partitioning potential seismic sources, analyzing the seismotectonics and estimating location of strong earthquakes.Due to the nonuniformity of earth media, instability of observation systems and disturbance of the environment, etc, the variety of observational data is complicated, that is, there is no absolutely "normal" or "abnormal", and seismic anomalies can be divided into many mutually exclusive "abnormal states". In different conditions of combined time-space-strength, determining seismic anomalies by different monomial forecast methods and its efficiency could be different due to the uncertainty of a precursor itself or complexity of the relationship between a precursor and earthquake gestation. It is very difficult to discover and dispose of this difference in actual application in a "two-state" model. But in a "multi-state" model, the difference can be easily reflected and the optimal combination of forecasting parameters for a forecast method can also be determined easily.Based on the "multi-state" precursory model and the optimization method for parameters of earthquake forecast model under the condition of optimal forecast efficiency, the relationship of the spatial location of earthquake with M≥6.0 and active faults in three seismic belts are analyzed. The results demonstrate that in the Hetao Seismic Belt, seismicity is mostly concentrated in the range of 20 km along the fault, the optimization model can forecast the location of potential earthquakes of M≥6.0 near the faults with a relatively high accuracy and the reliability is 0.5; while in the Qilian Mt. Seismic Belt, the reliability only reaches 0.14 when we use the model to estimate earthquakes within 30 km range along the faults. The "multi-state" precursory model, the efficiency-evaluating model and the parameter selection of individual earthquake forecast model based on optimal efficiency are of certain revelatory and practicable meanings for developing knowledge about precursors, investigating the laws of earthquake preparation and searching for optimal forecasting methods. 相似文献
9.
Surveys in Geophysics - 相似文献
10.
Ｉｎｖｅｓｔｉｇａｔｉｏｎｏｎｔｈｅｒｅｌａｔｉｏｎｂｅｔｗｅｅｎｔｈｅｇｒａｖｉｔｙａｎｏｍａｌｙ，ｃｒｕｓｔａｌｄｅｆｏｒｍａｔｉｏｎａｎｄｕｎｄｅｒｇｒｏｕｎｄｗａｔｅｒＸｕｅ－ＦａｎｇＷＵ（吴雪芳），Ｓｈｉ－ＨｕａＴＩＡＮ（田世华）ａｎｄＧｕ... 相似文献
11.
Liu Xiqiang 《中国地震研究》2005,19(2):181-191
Based on the Morlet complex wavelet transformation, the authors put forward a kind of new method for distinguishing periods of seismic activity and quietude and a new physical thought on the time-dependent wavelet accumulation energy spectrum with periods, the time-frequency distribution of wavelet vibration period spectrum and period-specific wavelet vibration spectrum. By applying the above methods to a time series which is composed of earthquake accumulation energy per year for the world, the Chinese continent and North China,respectively, we obtained some new information about the rhythm of shallow earthquake activity. Considering the historic earthquakes and the rhythm characteristics of current strong earthquake activity, the earthquake tendency in the next years is discussed. 相似文献
12.
An investigation on the temporal and spatial variation of ozone using the total column ozone (TCO) values during the cyclonic activities over North Indian Ocean (NIO) is carried out during the period from 1997 to 2012. The stepwise variation of TCO during the passage of the tropical cyclones over the Bay of Bengal and the Arabian Sea of the NIO is examined. The anomalies in TCO are estimated at each step of the life span of the cyclones starting from the genesis to landfall stages. The result reveals that the TCO values are quite high prior to the formation of the depression over NIO; however, at the stage of cyclogenesis it decreases which, with the increase in the intensity of the cyclones, further decreases and becomes minimum near the coast during the landfall. The maximum negative anomaly in TCO is observed for maximum intensity of the tropical cyclones as well as during the landfall. The result further shows that when the cyclones die out after the landfall the TCO regains the normal value. It is further observed that the reduction in TCO enhances the accumulated cyclone energy over NIO. The result finally shows that, the higher the energy of the cyclones, the lower becomes the stratospheric warming, that is, the higher the stratospheric cooling. 相似文献
13.
CAO Yonggang LIU Changjian LIU Tongmu FENG Yanqing LIU Yuqiang LIAO Shizhi CHEN Yizhan 《中国地震研究》2019,33(1):97-111
The coupling numerical model between astronomical tide and tsunamis was built based on the data of the COMCOT model, which was verified by the Japan "3·11" tsunami. The tsunami source of the Manila seismic tsunami was designed and computed to analyze the risk of tsunami which will happen in the Guangdong coast. According to the results, the maximum quantity of water increasing and the time of the tsunami arriving at the Guangdong seacoast were calculated. The coupling simulation between astronomical tide and tsunamis has significant meaning for evaluating the risk and early-warning of tsunamis in the Guangdong coastal area. 相似文献
14.
ＲｅｓｅａｒｃｈｏｎｔｈｅｓｅｉｓｍｏｇｅｎｉｃｅｎｖｉｒｏｎｍｅｎｔｆｏｒｄｅｅｐｅａｒｔｈｑｕａｋｅａｎｄｔｈｅｃａｕｓｅｏｆｅａｒｔｈｑｕａｋｅｓｉｎＸｉｎｊｉａｎｇａｎｄｉｔｓａｄｊａｃｅｎｔａｒｅａｓＱｉａｎｇＬＩ（李强）；Ｒｕｉ－Ｆｅｎｇ... 相似文献
15.
Ma Hongsheng 《中国地震研究》2006,20(3):232-243
INTRODUCTIONThe active blocks refer tothe geologic units that formedinlate Cenozoic (100 ~120 ka BP) andhave been highly active as fault zones since late Quaternary with relatively uniform motion styles(Zhang Guomin,et al .,2000 ;Zhang Peizhen,et al .,2003) .The active blocks are relativelyintactand have uniformmotion modalities ,their boundary zones (also called the active boundaries) are thelocalized or centralized zones of interactions and differential movement among the active block… 相似文献
16.
17.
Zheng Rongzhang 《中国地震研究》2004,18(4):385-395
The formation of strath and strath terrace is closely related to tectonic uplift in the drainage basin. Based on the investigation of straths at Yandantu and Changcaogou on the eastern segment of the northern margin fault of Altun, and in combination with the paleoclimatic data,the tectonic uplift since late Epipleistocene as revealed by stream terraces at the two places is discussed. At Yandantu, three levels of stream terraces( T1, T2 and T3 )have developed since 16ka BP, where T1, T3 and T2 are fill terraces and the buried major straths are exposed. The ages of three treads are dated to be about 16.1ka BP, 12 .Ska BP and 6.2ka BP, respectively. The three terraces reflect three tectonic uplift events, while the ages of the treads represent the occurrence time of these events. The stream is still beveling the bedrock and widening the channel at present, and the modern strath is being generated. The uplift rate is 4.8～4.5mm/a since 16.1 ka BP in this area. From 12.8ka B .P to 6.2ka BP, The uplift rate was 6.4mm/a.The uplift rate is 3. lmm/a since 6.2ka BP.At Changcaogou, four levels Of stream terraces(T1, T2, T3 and T1)have developed since 7ka BP. All of them are fill terraces. There are buried straths under the deposits. The buried major strath is exposed on T3 and T2 and the minor strath on T1‘and T1. The ages of treads of the three terraces (T3, T2 and T1’) are 7 ka BP, 3 ka BP and 2.5 ka BP, respectively. The four terraces reflect two uplift events induced by tectonic activities. One occurred in about 7 ka BP, and the other in 3ka BP. The uplift rate is 5.gmm/a since 7.0 ka BP at Changcaogou.From 7ka BP to 3ka BP, the uplift rate was 7.0mm/a, and since 3ka BP till now, the uplift rate is 4.7 mm/a. 相似文献
18.
Introduction Earthquake is not an isolated event. The focal region is not a closed system either. It is able to exchange energy or material with the medium outside this region. These kinds of exchange may cause various physical and chemical effects, so it is possible to get precursory signals by using space remote sensing technology. Many scholars (QIANG, et al, 1990; GENG, et al, 1992; XU, et al, 1995) have carried out some preliminary researches and experiments on the mechanism of therm… 相似文献
19.
Christian D. Klose 《Journal of Seismology》2013,17(1):109-135
A global catalog of small- to large-sized earthquakes was systematically analyzed to identify causality and correlatives between human-made mass shifts in the upper Earth??s crust and the occurrence of earthquakes. The mass shifts, ranging between 1?kt and 1?Tt, result from large-scale geoengineering operations, including mining, water reservoirs, hydrocarbon production, fluid injection/extractions, deep geothermal energy production and coastal management. This article shows evidence that geomechanical relationships exist with statistical significance between (a) seismic moment magnitudes M of observed earthquakes, (b) lateral distances of the earthquake hypocenters to the geoengineering ??operation points?? and (c) mass removals or accumulations on the Earth??s crust. Statistical findings depend on uncertainties, in particular, of source parameter estimations of seismic events before instrumental recoding. Statistical observations, however, indicate that every second, seismic event tends to occur after a decade. The chance of an earthquake to nucleate after 2 or 20?years near an area with a significant mass shift is 25 or 75?%, respectively. Moreover, causative effects of seismic activities highly depend on the tectonic stress regime in which the operations take place (i.e., extensive, transverse or compressive). Results are summarized as follows: First, seismic moment magnitudes increase the more mass is locally shifted on the Earth??s crust. Second, seismic moment magnitudes increase the larger the area in the crust is geomechanically polluted. Third, reverse faults tend to be more trigger-sensitive than normal faults due to a stronger alteration of the minimum vertical principal stress component. Pure strike-slip faults seem to rupture randomly and independently from the magnitude of the mass changes. Finally, mainly due to high estimation uncertainties of source parameters and, in particular, of shallow seismic events (<10?km), it remains still very difficult to discriminate between induced and triggered earthquakes with respect to the data catalog of this study. However, first analyses indicate that small- to medium-sized earthquakes (<M6) seem to be induced and large-sized events (>M6) seem to be triggered. The rupture propagation of triggered events might be dominated by pre-existing tectonic stress conditions. 相似文献