济阳坳陷东营三角洲前缘斜坡重力流成因砂体特征及形成条件

运用最新的深水重力流理论开展系统研究,细分大型三角洲前缘斜坡重力流成因砂体类型,并建立各类型砂体的判识标准,探讨砂体展布的控制因素。研究表明:大型三角洲前缘斜坡发育一系列重力流成因砂体,砂体并非由单一流体形成,包含了塑性体、砂质碎屑流及浊流等多种流体的有序转化和多个岩相组合;根据纵向上序列组合的差异,可把重力流砂体类型划分为滑动成因砂体、滑塌成因砂体、碎屑流成因砂体和浊流;利用岩心沉积构造特征、粒度特征、测井相和地震相等多角度对比可识别砂体类型;三角洲前缘斜坡重力流成因砂体的形成与展布受控于古物源、古沉积坡角、同沉积断层和沉积基准面旋回变化等因素,其中充足的物源是重力流砂体发育的物质基础、适宜的古坡角是重力流砂体有序展布的必要条件、同沉积断层下降盘是砂体发育的有利区,而基准面旋回变化决定了重力流砂体的纵向分布样式。     

气候变化下长三角城市群基础设施脆弱性评估及空间分析

城市基础设施是城市应对气候变化的关键环节。为了探究气候变化下城市基础设施系统的脆弱性及其空间分布特征,将脆弱性三要素理论与空间分析方法相结合,构建出气候变化下城市基础设施脆弱性的空间分析框架,并以长三角城市群各地级市为对象进行实证分析。通过脆弱性三要素的空间分布与空间相关性分析,发现三类要素的空间分布特征各异,脆弱性更多地取决于城市单元个体的行政级别、经济水平以及所属行政区域等因素,应将降低基础设施脆弱性的策略体系融入区域一体化政策中。     

Discovery of a 1.0 Ma Yellow River terrace and redating of the fourth Yellow River terrace in Lanzhou area

Based on the aeolian loess sequence-stratigraphic division and paleomagnetic datings on terraces, we found that an undiscovered terrace with the age of 1.0 Ma BP lies between the Dunwashan terrace and Wuyishan terrace. This terrace recorded an intensive Yellow River incision event during that period. Results of paleomagnetic dating and optically stimulated luminescence (OSL) dating of the Wuyishan loess section and Zaoshugou loess section on the fourth Yellow River terrace (T4) show that the age of the fourth Yellow River terrace in Lanzhou area is 0.86 Ma BP rather than the previously believed 0.6 Ma BP. This result answers a long-term question in the geomorphology community of whether there exists a 0.8 Ma terrace in Lanzhou area. The discovery of the 1.0 Ma Yellow River terrace and redating of the age of 0.6 Ma terrace in Lanzhou area provide new insights into further research on the evolution of Yellow River.     

2010—2020年长三角常住人口空间格局演变及影响因素研究

基于第6,7次区县尺度常住人口普查数据,分析了2010—2020年长三角地区人口空间格局的演变及其影响因素.研究发现：（1）长三角人口进一步向浙东北、苏南、浙西南集聚,上海、苏北和苏中地区常住人口比例有所下降;（2）长三角地级及以上城市划分为5个类型,其中杭州市、苏州市和宁波市为高增长型,上海市为中增长型,常州市、台州市和徐州市为低增长型,泰州市和淮安市为低减少型,盐城市为高减少型;（3）苏北、苏中地区人口向中心城区集聚,上海、南京、苏州等大城市的中心城区人口逐渐减少;（4）长三角常住人口规模空间演变影响因素复杂多变.基于研究结论,提出了相应政策建议.     

美姑河流域牛牛坝公路泥石流灾害防治

牛牛坝公路泥石流属于粘性泥石流,沉积区洪积扇典型,沉积物淤埋厚度12～25 m,泥石流在沉积区冲淤变动、加积特性显著,爆发周期3～5a.提出了泥石流隧道治理技术,拟定了治理结构方案,并进行了结构计算.以泥石流隧道附近的泥石流沟为对象,运用流-固耦合有限元数值模拟方法,分析了泥石流初始状态及峰值流量状态泥石流隧道及邻近泥石流沉积物内大主应力的变化规律,发现泥石流隧道顶部泥石流峰值流量出现8s以后沉积物及隧道结构内的大主应力才达到峰值.治理工程于2003年底修建完成,4a来经历了2次泥石流检验.现场观测发现,该防治工程治理效果显著.     

浅论江南丘陵城市环境特色的传承与发扬——以吉安市中心城市为例

针对当前快速发展的城市化进程中普遍存在的城市特色丧失的状况,阐述城市所处地域环境的唯一性是城市特色构成的关键元素。在归纳我国江南丘陵地带城市普遍具备的自然环境优势,并分析其对城市特色所起的作用后,结合吉安市的具体情况,提出了丘陵地带城市特色的传承与发扬的系列思考,包括城市腹地范围山水特色整体风貌与人文景观遗存的保护和利用;城区外围近郊背景圈中农村居民点规划和产业结构的调整;城区边缘城郊结合部的规划引导;城市片区之间的衔接过渡;城市街区环境特色创造以及具体的城市建设项目的实施等六个层面。     

松花江水污染模型的数值研究

研究参考文献[4]中干支流水系统所建立的反应扩散方程组.使用傅里叶级数方法,在不同条件下对此方程组的解进行数值模拟.     

SHRIMP zircon U-Pb dating for volcanic rocks of the Dasi Formation in southeast Hubei Province, middle-lower reaches of the Yangtze River and its implications

The Jinniu Basin in southeast Hubei,located at the westernmost part of middle-lower val-ley of the Yangtze River,is one of the important vol-canic basins in East China. Volcanic rocks in the Jin-niu Basin are distributed mainly in the Majiashan Formation,the Lingxiang Formation and the Dasi Formation,consisting of rhyolite,basalt and basaltic andesite,(trachy)-basalt and basaltic trachy-andesite and (trachy)-andesite and (trachy)-dacite and rhyolite respectively,in which the Dasi volcanism is volumet-rically dominant and widespread. The Dasi volcanic rocks were selected for SHRIMP zircon U-Pb dating to confirm the timing of volcanism. The results indi-cate that there exist a large amount of magmatic zir-cons characterized by high U and Th contents in the volcanic rocks. The concordia ages for 13 points are 128 ± 1Ma (MSWD = 3.0). On account of the shape of zircons and Th/U ratios,this age is considered to represent the crystallization time of the Dasi volcan-ism. The volcanic rocks in the Dasi,Majiashan and Lingxiang Formations share similar trace elementand REE partition patterns as well as Sr-Nd isotopic compositions. In combination with the regional geol-ogy,it is proposed that the southeast Hubei volcanic rocks were formed mainly during the Early Creta-ceous,just like other volcanic basins in middle-lower Yangtze valley. A lithospheric extension is also sug-gested for tectonic regime in this region in the Cre-taceous Period.     

赣江中游四大家鱼产卵场现状初步调查

为了解赣江中游四大家鱼产卵场现状,于2008年4月至2009年6月间通过现场采样和社会调查2种方法对赣江中游赣州至新干段12处四大家鱼产卵场进行了调查,并对水文和正在兴建的大型水利工程对产卵场的影响进行了分析。采得标本共计3 942尾,其中四大家鱼58尾;采集卵苗590尾,其中四大家鱼鱼卵38粒,获得51份渔民鱼类资源调查问卷。结果表明,20世纪60年代赣江中游原有12处产卵场中赣州储潭和峡江巴邱四大家鱼产卵场保存较好。