肥城市采煤塌陷地治理利用情况

1基本做法 肥城市地处山东中部，是山东省重要的煤炭基地，自1958年建矿以来，先后有13座煤矿建成投产。地下煤炭资源的开采，造成大面积土地塌陷，严重破坏了矿区的地形地貌。塌陷涉及肥城市4个镇71个行政村，总面积5000hm^2。由于地面塌陷，交通、水利、农业基础设施遭到严重破坏，大面积的粮田成为沼泽水域，杂草丛生，荆棘遍地，生态环境恶化，人民的正常生产和生活受到重大影响。     

布袋注浆桩在深厚层软土地基加固中的应用

布袋注浆桩是一项新的软土地基加固技术,应用于深厚层和夹硬层的软土加固,具有明显的优势。结合甬台温铁路深厚层软土地基加固,介绍了布袋注浆桩的加固机理、设计、施工、质量检测方法和标准等。检测结果表明,布袋注浆桩成桩质量良好,加固后,地基沉降得到有效控制,满足设计要求。     

Cosmogenic Be inferred lake-level changes in Sumxi Co basin, Western Tibet

Most Tibetan lakes are surrounded by conspicuous regressive shorelines attesting to high-water levels in the past. Concentrations of the in situ produced cosmogenic radionuclide ¹⁰Be in bedrock from the three highest terraces surrounding Sumxi Co, situated in Western Kunlun, indicate that the highest lake-level appeared before 10,000–11,500 yr, and most likely between 11,000 and 12,800 yr. Younger ages for the two lower terraces imply regression of Sumxi Co during the early-mid Holocene. The concurrency of the highest lake-level with orbitally induced maximum northern hemisphere summer insolation suggests that the increase in water supply to Sumxi Co was most likely associated with increased recharge from melting glaciers. We conclude that the enhanced Indian monsoon during the early Holocene did not penetrate the Tibetan plateau and affect the northwestern part of Tibet significantly.     

Single epoch ambiguity resolution for Galileo with the CAR and LAMBDA methods

This paper investigates single epoch ambiguity resolution performance using Galileo four frequency data. Two commonly used ambiguity resolution methods are used in the tests, including the Cascade Ambiguity Resolution (CAR) and the Least-Squares Ambiguity Decorrelation Adjustment (LAMBDA) methods. For CAR method, four optimal combinations are carefully selected according to their wavelength to noise ratios and success rate for ambiguity fixing. The test results show, in general, the LAMBDA method performs better than the CAR method. The speed of ambiguity resolution is closely related to the carrier phase measurement precision. With carrier phase measurement precision of 3 mm, single epoch ambiguity resolution can be achieved at every epoch with simulated 1-s interval 24-h Galileo data (total epochs 86,400). With the increase of carrier phase noise, ambiguity resolution performances become worse. When the noise level is increased to 12 mm, single epoch ambiguity resolution can only be achieved about 50% of epochs.     

India-Eurasian collision vs. ocean-continent collision＊

Introduction Major tectonic activities occur in collisions zones between plates or intra-plate continental blocks. Therefore, it is significant to investigate collision processes. We know that orogenic and seismic belts in plate margins are closely relate…     

河北邢台余震窗地震活动对华北地区6级以上地震的预测反应

文中简要介绍了1966年河北邢台地震发震的构造背景。在选取合理的地震参数确立余震窗后,分析了余震窗地震月频次的变化特征对研究华北地区6级以上地震的反应。发现,余震活动出现月频次过程异常对应华北地区6级地震成组活动或震群活动;单点高值频次异常则对应单发6级地震。     

Erosion in northwest Tibet from in‐situ‐produced cosmogenic 10Be and 26Al in bedrock

Concentrations of in‐situ‐produced cosmogenic nuclides ¹⁰Be and ²⁶Al in quartz were measured by accelerator mass spectrometry for bedrock basalts and sandstones located in northwest Tibet. The effective exposure ages range between 23 and 134 ka (¹⁰Be) and erosion rates between 4·0 and 24 mm ka^?1. The erosion rates are significantly higher than those in similarly arid Antarctica and Australia, ranging between 0·1 and 1 mm ka^?1, suggesting that precipitation is not the major control of erosion of landforms. Comparison of erosion rates in arid regions with contrasting tectonic activities suggests that tectonic activity plays a more important role in controlling long‐term erosion rates. The obtained erosion rates are, however, significantly lower than the denudation rate of 3000–6000 mm ka^?1 beginning at c. 5‐3 Ma in the nearby Godwin Austen (K2) determined by apatite fission‐track thermochronology. It appears that the difference in erosion rates within different time intervals is indicative of increased tectonic activity at c. 5–3 Ma in northwest Tibet. We explain the low erosion rates determined in this study as reflecting reduced tectonic activity in the last million years. A model of localized thinning of the mantle beneath northwest Tibet may account for the sudden increased tectonic activity at c. 5–3 Ma and the later decrease. Copyright © 2006 John Wiley & Sons, Ltd.     

北京地区暖季对流天气的气候特征

对北京地区最近12年暖季(5—9月)雷暴、冰雹、暴雨和大风等各种对流天气进行了气候统计和分析。统计结果表明:北京地区暖季发生对流的概率很高,按日数统计的气候概率达47.77%,大风、暴雨和冰雹气候概率分别为27.29%、10.84%和6.29%。暴雨多发季节为7月中旬到8月上旬。冰雹集中于6月中、下旬。在对流天气的地理分布上,北京西北部、东北部山区及西南部山区多对流天气,中心区和东南部平原地区对流天气较少。暴雨呈西南—东北方向带状分布,东北部山区、中部和东南部平原地区多发生暴雨,而西北部和西南部山区很少发生暴雨。山区冰雹明显多于平原。西北部和东北部山区大风偏多。暴雨有明显的夜发性。冰雹集中发生在午后到傍晚,占冰雹总站次的76.72%。     

Compositions of heavy minerals in Northeastern China sandlands and provenance analysis

Sand samples deposited since the Last Glacial Maximum (LGM) from the Hulun Buir, Horqin and Otin-dag sandlands were measured for their assemblages of heavy minerals and chemical compositions of detrital garnets and tourmalines. Heavy mineral assemblages of these three sandlands consist mainly of garnet, ilmenite, epidote and minor amphibole and magnetite. Garnets consist mainly of high Mg type-A ones (58% on average), and minor type-B ones. Toumalines are mainly composed of Mg-rich and minor Fe-rich ones. Compared with those of central-southern Mongolia and central Tarim, these three sandlands are derived from the Phanerozoic rocks of the Central Asian Orogenic Belt and the Archean and Paleoprotorozoic basement rocks of the North China Craton. Our results provide direct evidence that the present-day sands may be reworked from LGM ones. Differences of heavy mineral composi-tions occur between the samples of the three sandlands and Taklimakan Desert, indicating that the material of the western arid regions contributes little to the eastern sandlands.