DETERMINATION OF SLIP RATE ON THE SOUTHERN SEGMENT OF THE ANNINGHE FAULT     

WANG Hu  RAN Yong-kang  CHEN Li-chun  LIANG Ming-jian  GAO Shuai-po  LI Yan-bao  XU Liang-xin 《地震地质》2018,40(5):967-979

The Anninghe Fault has been suggested as an important segment of the fault system along the eastern boundary of the Sichuan-Yunnan faulted block in the southeastern region of the Tibetan plateau. Reliable determination of the Late Quaternary slip rate on the Anninghe Fault is very helpful and significant for revealing deformation mechanism and kinematic characteristics of the Sichuan-Yunnan faulted block, which further helps us understand fault activity and seismic potential of the region. However, previous studies were focused mainly on the northern segment of the Anninghe Fault, while slip rate on its southern segment has been less studied. Therefore, in this paper, we chose two sites at Dashuigou and Maoheshan on the southern segment of the Anninghe Fault, and used high-resolution images of unmanned aerial vehicle (UAV)photogrammetry technology, detailed field survey, multiple paleoseismic trenching and radiocarbon dating methods to constrain slip rate on the southern fault segment of the Anninghe Fault. Specifically, we suggest that the slip rate at the Dashuigouo site is narrowly constrained to be~4.4mm/a since about 3^￣￣300a^￣￣BP based on a linear regression calculation method, and speculate that a slip rate of 2.6~5.2mm/a at the Maoheshan site would be highly possible, although we poorly constrained the whole deformation amount of the two branch faults at the Maoheshan site from multiple paleoseismic trenching. The data at the two sites on the southern segment show a consistent slip rate compared with that of the northern segment of the Anninghe Fault. Moreover, considering a similar paleoseismic recurrence interval on the two segments of the Anninghe Fault from previous studies, we further suggest that the fault activity and deformation pattern on the two segments of the Annignhe Fault appears to be well consistent, which is also in agreement with the regional tectonic deformation.  相似文献   

塔里木盆地东北缘晚新生代钻孔岩心磁性地层年代学及其构造意义          下载免费PDF全文

杨吉龙  胥勤勉  袁海帆  谢宁  白铭  胡云壮  田立柱 《地球物理学报》2018,61(10):4075-4087

塔里木盆地的高分辨率沉积记录对于理解青藏高原隆升、亚洲内陆干旱化乃至全球气候变化至关重要.建立可靠的地层年代标尺对于研究塔里木盆地晚新生代沉积环境演化、构造运动及古气候变化具有重要意义.本文对塔里木盆地东北缘库尔勒地区的两个全取心钻孔ZK3（深500 m）、ZK5（深300 m）进行详细的磁性地层学研究，结果表明，ZK3孔中更新统底界为54.8 m，下更新统底界为167.0 m，上新统底界为432.0 m，钻孔底部年龄约为6.2 Ma，属上中新统上部；ZK5孔中更新统底界为64.7 m，下更新统底界为241.5 m，钻孔底部年龄约为3.2 Ma，属上上新统.基于上述磁性地层年代标尺，通过沉积速率分析发现ZK3孔在3.0—3.6 Ma之间沉积速率明显增大，反映了塔里木盆地北部天山在此期间的快速隆升.通过东西部多个盆地地质剖面沉积速率的对比分析发现，这期构造活动在区域上具有准同期活动特征，在时代上与晚中新世以来青藏高原快速隆升的时代一致，可能与青藏高原的隆升扩展效应有关.  相似文献   

Self-thinning Rules at Chinese Fir (Cunninghamia lanceolata) Plantations—Based on a Permanent Density Trial in Southern China     

DUAN Aiguo  FU Lihua  ZHANG Jianguo 《资源与生态学报(英文版)》2019,10(3):315-323

Data selection and methods for fitting coefficients were considered to test the self-thinning law. The Chinese fir (Cunninghamia lanceolata) in even-aged pure stands with 26 years of observation data were applied to fit Reineke’s (1933) empirically derived stand density rule (N $propto$ d¯ ^-1.605, N = numbers of stems, d¯ = mean diameter), Yoda’s (1963) self-thinning law based on Euclidian geometry (v¯ $propto$ N ^-3/2, v¯ = tree volume), and West, Brown and Enquist’s (1997, 1999) (WBE) fractal geometry (w¯ $propto$ d¯ ^-8/3). OLS, RMA and SFF algorithms provided observed self-thinning exponents with the seven mortality rate intervals (2%-80%, 5%-80%, 10%-80%, 15%-80%, 20%-80%, 25%-80% and 30%-80%), which were tested against the exponents, and expected by the rules considered. Hope for a consistent allometry law that ignores species-specific morphologic allometric and scale differences faded. Exponents α of N $propto$ d¯^α, were significantly different from -1.605 and -2, not expected by Euclidian fractal geometry; exponents β of w¯ $propto$ N^β varied around Yoda’s self-thinning slope -3/2, but was significantly different from -4/3; exponent γ of w¯ $propto$ d¯^γ tended to neither 8/3 nor 3.  相似文献   

青藏高原土壤水分变化对近地面气温的影响     

范科科  张强  孙鹏  宋长青  余慧倩  朱秀迪  申泽西 《地理学报》2020,75(1):82-97

青藏高原为全球气候变化最为敏感的区域之一,探讨该地区土壤水分变化对近地面气温的影响将为青藏高原水汽循环研究及该地区对周边气候与环境的影响研究提供重要理论支撑。利用NCEP-CFSR数据集,基于土壤水分对近地面气温的影响机理,揭示了青藏高原不同季节、不同植被分区下土壤水分时空分异规律、土壤水分与蒸发率的响应与耦合状态及土壤水分通过蒸散发过程对近地面气温的影响。结果表明：① 不同季节下青藏高原土壤水分空间分布基本一致,除西北地区和喜马拉雅山脉外,整体呈现由东南向西北递减趋势,青藏高原地区存在干旱区变湿,湿润区变干的空间特征;② 青藏高原大部分区域土壤水分处于干湿过渡状态,其中青藏高原南部和东南部地区全年处于干湿过渡状态,而柴达木盆地几乎全年处于干旱状态;③ 近地面气温对土壤水分的响应在冬季最弱,在夏季最强且空间差异较小,其中在冬、春、夏季为负反馈,另外不同植被覆盖区近地面气温对土壤水分的敏感性差异很大。此项研究对于进一步探讨青藏高原地区陆气耦合状态及变化环境下的区域水汽循环及其效应具有重要理论意义。  相似文献   

流量对水力压裂破裂压力和增压率的影响研究     

邵长跃  潘鹏志  赵德才  姚天波  苗书婷  郁培阳 《岩土力学》2020,41(7):2411-2421

水力压裂现场原位测试试验的破裂压力是计算构造地应力的重要参数。为了探究流量对水力压裂破裂压力和增压率的影响，设计4种不同恒定流量情况的低渗透硬脆灰岩室内大型水力压裂试验，结合声发射监测技术分析不同流量下水力裂缝破裂压力、破坏模式和缝网复杂程度的规律以及流量与增压率的内在关系。试验结果表明：流量越大，破裂压力越高，缝网复杂程度越低；典型压力?时间曲线分为缓慢增压段、急速增压段、稳定增压段和突然下降段；稳定增压段增压率保持不变，压力随时间线性增长，其增压率的大小和流量存在明显的线性关系；基于流量与稳定增压段增压率的线性关系，考虑流量因素的Ito理论可以很好地定量解释流量对破裂压力的影响，试验结果与理论预测吻合度较高。  相似文献   

人民币汇率升值对海洋产业的非对称效应研究          下载免费PDF全文

李宁 《海洋开发与管理》2020,37(6):70-75

文章基于协整分析方法，研究人民币汇率升值对我国海洋产业产生的影响，结果表明：人民币汇率升值会对海洋第一产业产生负向效应，而对海洋第二、第三产业的影响则不显著。选择海洋渔业、海洋旅游业等七大海洋产业，利用VAR模型分析人民币汇率升值对各个海洋产业产生的非对称效应。总体来看，各海洋产业对人民币汇率升值均表现出负向响应，从侧面验证人民币汇率升值对海洋产业结构影响的分析结论。最后提出未来海洋经济发展要关注人民币汇率等政策建议。  相似文献   

五大连池老黑山火山钾质玄武岩结晶动力学研究     

彭年  崔莹  刘永顺  乔学斌  朱晓艳  聂保锋  胡亚朵 《岩石学报》2020,36(7):2035-2046

本文模拟了五大连池地区老黑山火山钾质响质碱玄岩熔岩在不同降温速率下从1150℃冷却到700℃橄榄石的结晶动力学过程,并从晶体粒度、晶体数量和晶体形态三方面研究了晶体结晶特征与降温速率之间的关系。结果表明:(1)晶体粒度分布(CSD)显示七组不同降温速率下的晶体粒度与布居密度均呈现较好的幂率关系,且幂律指数相近,斜率范围在3.69～4.42之间,这说明了晶体粒度分布对降温速率的依赖性并不显著。(2)随着降温速率由快变慢,晶体数量总体增长。当降温速率为0.0468℃/min时,晶体数量达到峰值。随后,结晶进入以退火合并为主的晶体粗化过程,直至结晶动力学达到平衡。(3)各降温速率下晶体形态呈现出分形特征,分形维数界于1.39～1.62之间,反映了新生晶体生长的自组织临界性。不同降温速率下的晶体边界复杂程度出现较大无规波动,显示出晶体形态对降温速率的高度敏感性。当降温速率为0.1℃/min时,晶体边界形态最复杂,当降温速率变慢到0.0468℃/min后,晶体边界形态的复杂程度趋于稳定。本项动力结晶实验对于深入了解五大连池新期火山熔岩流的运动机制以及动力结晶过程有重要的科学意义。  相似文献   

大菱鲆卵子排放后在卵巢腔内老化特征初探     

宋宗诚  王学颖  薛蕊  肖志忠  马道远  刘清华  李军 《海洋科学》2019,43(7):106-111

为了探明大菱鲆(Scophthalmus maximus)卵子在卵巢腔内老化的原因及特征,采用连续跟踪采卵的方式,通过荧光染色、生理生化指标测定,对不同采卵时间(0, 3, 6, 9, 12 h)的卵子活性氧和脂质过氧化情况(氧化产物丙二醛MDA)、抗氧化系统(超氧化物歧化酶SOD,还原型谷胱甘肽GSH)、卵巢液pH值及受精率和孵化率进行对比研究。结果表明,随着卵子在体内老化时间的延长,其活性氧含量及脂质过氧化程度逐渐升高,活性氧含量及过氧化程度与排卵后卵子老化呈正相关;SOD酶活力,GSH酶活力均显著下降,MDA含量显著提高;受精率和孵化率均显著下降。排卵后6h,孵化率降到2.87%～10.60%,此时的卵质已经极度恶化,不能再继续用于后续的生产中。综上,在卵巢腔中,卵子排放后,随着时间的延长,活性氧含量显著升高,抗氧化能力逐渐下降,受精率和孵化率显著降低,老化逐渐加剧。  相似文献   

The dynamics of mountain erosion: Cirque growth slows as landscapes age     

Iestyn D. Barr  Jeremy C. Ely  Matteo Spagnolo  Ian S. Evans  Matt D. Tomkins 《地球表面变化过程与地形》2019,44(13):2628-2637

Glacial cirques are widely used palaeoenvironmental indicators, and are key to understanding the role of glaciers in shaping mountain topography. However, notable uncertainty persists regarding the rate and timing of cirque erosion. In order to address this uncertainty, we analyse the dimensions of 2208 cirques in Britain and Ireland and model ice accumulation to investigate the degree of coupling between glacier occupation times and cirque growth. Results indicate that during the last ~120 ka, cirques were glacier-free for an average of 52.0 ± 21.2 ka (43 ± 18%); occupied by small (largely cirque-confined) glaciers for 16.2 ± 9.9 ka (14 ± 8%); and occupied by large glaciers, including ice sheets, for 51.8 ± 18.6 ka (43 ± 16%). Over the entire Quaternary (i.e. 2.6 Ma), we estimate that cirques were glacier-free for 1.1 ± 0.5 Ma; occupied by small glaciers for 0.3 ± 0.2 Ma; and occupied by large glaciers for 1.1 ± 0.4 Ma. Comparing occupation times to cirque depths, and calculating required erosion rates, reveals that continuous cirque growth during glacier occupation is unlikely. Instead, we propose that cirques attained much of their size during the first occupation of a non-glacially sculpted landscape (perhaps during the timeframe of a single glacial cycle). During subsequent glacier occupations, cirque growth may have slowed considerably, with the highest rates of subglacial erosion focused during periods of marginal (small glacier) glaciation. We propose comparatively slow rates of growth following initial cirque development because a ‘least resistance’ shape is formed, and as cirques deepen, sediment becomes trapped subglacially, partly protecting the bedrock from subsequent erosion. In support of the idea of rapid cirque growth, we present evidence from northern British Columbia, where cirques of comparable size to those in Britain and Ireland developed in less than 140 ka. © 2019 John Wiley & Sons, Ltd. © 2019 John Wiley & Sons, Ltd.  相似文献   

基于GPS观测的天津地区形变应变场与构造活动     

纪静  郭良迁  张文朋 《大地测量与地球动力学》2018,38(6):614-619

2006~2015年天津地区GPS连续观测站形变和应变计算结果显示，天津地区形变场和应变率场变化复杂，存在南北分带和东西分带特征。天津地区形变场和应变场主要受控于唐山-磁县地震构造带和张家口-渤海地震构造带等多组活动断裂的切割作用。  相似文献