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运用LAICPMS技术,对内蒙古乌兰敖包地区原“阿木山组”之上所采集的流纹质凝灰熔岩样品进行锆石UPb测年,获得19个有效数据,年龄范围分布为(248±5)~(277±5)Ma,主要峰值263~248Ma(17个数据),另有2个数据为273Ma、277Ma与其他17个数据不协调,这可能是岩浆从外部带入的早期结晶锆石。根据样品岩石学特征及UPb年代学特征,结合区域构造演化等,分析认为研究区在晚二叠世早期(255.2±2.4)Ma有一定规模的熔岩喷发,该套海相火山碎屑岩层位与银额盆地北部地区哈尔苏海组地层相当,可归入哈尔苏海组。 相似文献
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该文详细论述了鲁北地区水文地质条件、工程地质条件。以多期水准测量数据为基础,以校验后的多年insar解译数据辅助,获取了鲁北地区地面沉降速率及多年累积地面沉降量。结果表明,鲁北平原年沉降速率大于50mm/a的地区面积502.73km~2,区内存在2个显著的沉降中心,一个位于德州市城区西北部张庄,地面累积沉降量超过1.3m,一个位于广饶县县城东北部,多年地面累积沉降量达1.605m,200mm沉降等值线圈闭面积14 904km~2,占鲁北平原区面积的34.34%。分析了鲁北平原地区地面沉降机理,建立了地面沉降与地下水水位相关关系,并针对现状问题提出了防治措施与建议。 相似文献
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【目的】研究南海北部近海区域柱状沉积物多环芳烃组成及分布特征,讨论全新世早期火历史及气候变化。【方法】利用AMS 14C定年技术结合有机地球化学分析手段对全新世早期南海北部近海沉积物柱状样品中多环芳烃(PAHs)分布特征进行研究。【结果】南海北部近海沉积物中16种PAHs总浓度范围为8.58~17.48 ng/g,在约10000 a B.P.的全新世早期呈现先增大后减小波动变化,与TOC变化基本同步。【结论】沉积物中多环芳烃主要来源于南海北部近海陆源区域自然火灾产生的焦炭残渣。PAHs的沉积浓度变化间接指示了全新世早期东亚季风的强度变化。 相似文献
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模拟湛江港涉海工程施工产生的悬浮物,探讨底泥悬浮物对工程附近海区近江牡蛎养殖的影响,研究不同浓度悬浮物对大、小规格近江牡蛎(Crassostrea rivularis)的毒害效应。结果表明,悬浮物对大规格近江牡蛎(8.12±1.76 cm)的毒害影响不明显;对小规格近江牡蛎(2.33±0.78 cm),悬浮物浓度≤270 mg/L时死亡率低于30%,悬浮物浓度≥810 mg/L时死亡明显增加,死亡率达60%。通过概率单位法计算,小规格近江牡蛎的96 h半致死浓度为627.17 mg/L。 相似文献
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刘钧枢 《地球科学与环境学报》1994,(4)
根据对Z_(37-2)孔的孢粉分析结果表明,郑州地区,自全新世以来,气候经历三次较大的波动,先是气候开始转暖,气温不高,温凉半湿润;二是气候继续升高,达到“最适宜”气候期,温暖湿润;最后是气候再度下降,降水减少,温凉偏干.本区气侯变化规律,与北京地区基本符合.依据气侯地层学的观点,并结合放射性碳年代测定,本区的全新世地层可以划分为三期:即全新世早期(距今11000~7500a),全新世中期(距今7500~2500a),全新世晚期(距今2500a至今). 相似文献
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《青岛海洋大学学报(英文版)》2014,(1):83-90
Nutrient enrichment experiments with nitrogen (N) and phosphorus (P) were conducted with samples from two stationsin the coastal waters of Qingdao, China, during summer to identify limiting nutrients. In late July of 2009, low P concentrations andthe maximum photochemical efficiency of photosystem II (Fv/Fm) in the initial samples together with Fv/Fm and chlorophyll a (Chl a)responses to P addition indicated P limitation at the two stations. In early August, low P levels still limited phytoplankton growth atstation A. Fv/Fm and Chl a were the highest in the NP treatments at station B, suggesting an N/P co-limitation. In mid-September,nutrient concentrations and Fv/Fm were elevated and phytoplankton communities were healthy. Greater Fv/Fm and Chl a in the treat-ments with added P than those without the addition suggested potential P limitation at station A. Lack of Fv/Fm and Chl a responsesfollowing nutrient additions indicated N and P repletion at station B. At the end of July 2010, neither N nor P was limited at station B.Additionally, Fv/Fm coupled with 24-h-long nutrient enrichment experiments can be used to detect P limitation and N/P co-limitationto natural populations. This method can be more accurate for assessing co-limitation than the use of criteria of nutrient concentrationsand ratios as indicators, and can provide more rapid results than nutrient addition bioassays using chlorophyll response as an indica-tor, when a population is potentially limited. Compared with the two conventional methods, the results based on F,/F~ can also pro-vide more detailed information about physiological states of the populations. 相似文献
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【目的】研究香港牡蛎(Crassostrea hongkongensis)对低氧的耐受性及复氧后的恢复能力,为香港牡蛎养殖及耐低氧品系选育提供参考。【方法】开展溶解氧分别为0.5、1.5、2.5 mg/L低氧胁迫72 h及复氧24 h的实验,分析其鳃、闭壳肌的抗氧化能力及能量代谢相关酶活性的变化情况。【结果】1)低氧胁迫6 h时,0.5 mg/L及1.5 mg/L两组香港牡蛎总抗氧化能力(T-AOC)、糖原含量、丙酮酸激酶(PK)活性和磷酸果糖激酶(PFK)活性显著降低(P <0.05),磷酸烯醇式丙酮酸激酶(PEPCK)活性与对照组差异不显著(P> 0.05);2)低氧胁迫72 h时,T-AOC、糖原含量以及能量代谢酶PK、PFK、PEPCK活性显著升高(P <0.05);3)复氧24 h后,1.5 mg/L和2.5 mg/L两个低氧组牡蛎的T-AOC,PK酶及PFK酶活性基本恢复至初始水平,与对照组相比差异不显著(P> 0.05),0.5 mg/L低氧组牡蛎各项指标仍显著低于对照组,3个低氧组PEPCK酶活性均显著高于对照组(P <0.05)。【结论】... 相似文献
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黄河三角洲高效生态经济区是具有国家战略地位的重要生态经济区,该地区的海岸带地处海陆交接地带,属于陆缘海海岸带,生态环境脆弱,区域海岸带地形地貌系统性阐述甚少。在开展该区域生态地质环境调查的基础上,结合实际调查情况及以往文献的研读,对该地区海岸带地形地貌、岸滩地貌类型及特征进行了系统性归纳总结。整个黄河三角洲高效生态经济区的海岸带地貌分黄河三角洲粉砂淤泥质海岸、莱州湾南岸潍北平原区粉砂淤泥质海岸、莱州砂质海岸3个部分。岸滩类型分为黄河三角洲岸段冲淤平衡潮滩、侵蚀潮滩、淤积潮滩3种及莱州湾岸段侵蚀潮滩及侵蚀砂质海滩2种。 相似文献
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Relevant geological, geographical, archaeological data were collected to study the characteristics of middle Holocene warm period and sea level high on North China coast. Middle Holocene climate and sea level change on North China coast were correlated to warm marine environment events in about 8-3 ka B.E The sea level in about 8 ka B.E was higher than present mean sea level, then fluctuated for 5 000 years and after that it became even in 3 ka B.E The highest sea level occurred in about 6-5 ka B.E; the maximum was about 2-3 m and minimum was about 1-2 m. 相似文献
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Based on the new data of the Quaternary along the coast of Hainan Island, China, this paper puts forward that the Holocene in Hainan Island can be divided into four formations: Wanning formation (Q41), Sanya formation (Q42-1), Qiongshan formation (Q42-2) and Ledong formation (Q43). Spore-pollen analysis shows that there are 6 spore-pollen zones existed, reflecting two cycles of climatic fluctuation from warm-dry to hot-humid. The climax of hot-humid period occurred 6,000-5,000 years B.P.. Based on the 14C dating data of the 38 samples representing the positions of ancient sea level, a breakthrough curve representing the sea level change during the Holocone is obtained, in which , a sea level change caused by tectonic movement is subtracted. Two cycles of rise-drop of sea level with three periods of high sea level were found. The period with the highest sea level is some 6,000-5,000 years B.P.. According to the rise-drop rate of sea level, four periods of the sea level change can be distinguished in the 相似文献
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ImODUcrIONGroundwaterwthAnneralimtionofmorethan5OgA(about5"Be')"iscalledunder-groundbrine.ltbelongstoevaporationoredepositinliquidstateandisantwortantrnaterialsourceforsaltonkingandthechewhcalindustry.QuatemarylittoralfadesundergroundbrinewasstoredinthelittoralsoneandhadtwobasictypesofgenesisenvironmentflittoralplaincoastenvironmentcharacterindbythecoastalongLaichouBay,andembayedcoastenvironmentcharaCterindbythecoastalzoneofQingdao.TheauthorresearchedthebrineintheLaizhoubaycoastareainthe… 相似文献
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《中国海洋湖沼学报》2019,(6)
Sea level rise is a slow-onset disaster. We collected information about the natural and ecological environments, tides and sea levels, and socio-economic aspects to investigate the distribution and zoning of the risks from sea level rise across Shandong Province. The trends in sea level in different counties of Shandong Province were predicted using moving averages and a random dynamic analysis forecasting model, and the model outputs and socio-economic indicators were combined to assess the risks. The results show that the risks of sea level rise along the western coast of Bohai Bay and Laizhou Bay in Shandong Province were sufficiently large to warrant attention. 相似文献
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In this study, we used Landsat images and meteorological data to examine the spatiotemporal distribution and variability of sea ice in Jiaozhou Bay(JZB) between 1986 and 2016. The results show that JZB is not always covered by sea ice in winter, but in some extreme cases, sea ice has covered more than one-third of the sea area of the bay. Sea ice in JZB has generally formed between January 1 and February 5, primarily along the coast, and gradually expanding to the central area of the bay. Both meteorological and artificial factors have played important roles in modulating the sea ice distribution. We found sea ice coverage to have been strongly correlated with the accumulated freezing-degree days nine days before the occurrence of sea ice(R2 = 0.767). North-northwest surface winds have dominated the freezing period of sea water in the JZB, and wind speed has exerted a more significant influence on the formation of sea ice when the sea ice coverage has been generally small. Additionally, artificial factors began to affect the expansion of sea ice in JZB since 2007. The construction of the Jiao-Zhou-Bay Bridge(JZBB) is believed to have retarded water flow and reduced the tidal prism, thereby leading to the formation of an ice bridge along the JZBB, which effectively prevents the southward expansion of sea ice. 相似文献
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The 2nd Member of Kongdian Formation has been made up of a large number of oil shale and mudstone in the Kongnan aera of Huanghua depression around the Bohai Bay. In the Kongnan area, the lake basins were very large and deep during the deposition of the 2nd Member of Kongdian Formation. During that period,the lakes were sealed, uncommunieated with the sea water and the paleoclimate was very warm and wet in Kongnan area. Analyzing the content of the trace element and the rare earth element, carbon and oxygen isotope in the disquisition, The authors prove the two views correct. 相似文献
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Qinghua YAN Jing SUN Xudong ZHANG Qinglong MENG Man WANG 《东北亚地学研究》2007,10(1):48-54
The 2nd Member of Kongdian Formation has been made up of a large number of oil shale and mudstone in the Kongnan aera of Huanghua depression around the Bohai Bay.In the Kongnan area,the lake basins were very large and deep during the deposition of the 2nd Member of Kongdian Formation.During that period,the lakes were sealed,uncommunicated with the sea water and the paleoclimate was very warm and wet in Kongnan area.Analyzing the content of the trace element and the rare earth element,carbon and oxygen isotope in the disquisition,The authors prove the two views correct. 相似文献