ACCRETION OF AN EARLY CRETACEOUS INTRA- OCEANIC ISLAND ARC TO INDIA: EVIDENCE FROM THE YARLUNG ZANGBO SUTURE ZONE

ACCRETION OF AN EARLY CRETACEOUS INTRA- OCEANIC ISLAND ARC TO INDIA: EVIDENCE FROM THE YARLUNG ZANGBO SUTURE ZONE     

内蒙古锡盟——赤峰北部板块构造演化与金矿床

研究区位于西伯利亚板块与华北板块的接合部位,是由锡林浩特“微板块”和一系列缝合线组成。构造演化经历了两次大的“开合”运动和两期“活化”。前者为金矿提供成矿物质;后者使之进一步富集成矿。根据其构造演化和成矿特征,提出本区主要有４类金矿床。     

扬子板块西缘黄草山和下索子花岗岩体锆石U-Pb年代学研究

对扬子板块西缘泸定—石棉地区黄草山花岗岩体和康定地区下索子花岗岩体中自形锆石,采用205Pb-235U混合同位素稀释法测定了锆石U-Pb年龄。测试结果表明,黄草山岩体中锆石结晶年龄为786±36Ma,下索子岩体中锆石结晶年龄为805±15Ma,表明它们都是晋宁期岩浆活动产物。     

载荷试验有限元数值模拟

载荷试验是目前世界各国用以确定地基承载力的最主要方法,在地基处理效果检验中被广泛采用,然而载荷试验在实际操作过程中也存在不少问题,如尺寸效应、费用高、工期长等。新兴的有限元等数值方法克服了以往耗时量大、操作复杂、精度不足等缺点,已逐渐成为岩土工程领域有效的实用计算方法。鉴于上述原因,尝试用增量加载有限元法对载荷试验进行数值模拟。算例结果表明,只要强度参数与实际情况相符,载荷试验的结果可以通过有限元模拟获取。     

双参数地基上弹性板的动力分析

采用双参数地基模型和基于Mindlin板理论的8节点等参单元,根据Hamilton变分原理,推导了弹性地基上弹性板动力分析的有限元公式,将地基效应和板面质量分布归并到板的刚度矩阵和质量矩阵中,采用边界元法考虑板域外地基变形的影响。分析了四边自由矩形板的自由振动和强迫振动,计算的自由振动固有频率与实测结果相近,发生共振时板的强迫振动动力响应达到峰值,在给定的阻尼比条件下,无阻尼的稳态响应与有阻尼的稳态响应趋于相同,阻尼能够显著降低板的共振响应。     

旅游规划理论的结构

该文阐述旅游规划理论体系的结构,旨在解决众多理论之间的“接口”问题。     

Imaging crustal discontinuities and the downgoing slab beneath western Crete

The migration of teleseismic receiver functions yields high-resolution images of the crustal structure of western Crete. Data were collected during two field campaigns in 1996 and 1997 by networks of six and 47 short-period three-component seismic stations, respectively. A total of 1288 seismograms from 97 teleseismic events were restituted to true ground displacement within a period range from 0.5 to 7 s. The application of a noise-adaptive deconvolution filter and a new polarization analysis technique helped to overcome problems with local coda and noise conditions. The computation and migration of receiver functions results in images of local crustal structures with unprecedented spatial resolution for this region. The crust under Crete consists of a continental top layer of 15–20 km thickness above a 20–30 km thick subducted fossil accretionary wedge with a characteristic en echelon fault sequence. The downgoing oceanic Moho lies at a depth of 40–60 km and shows a topography or undulation with an amplitude of several kilometres. As a consequence of slab depth and distribution of local seismicity, the Mediterranean Ridge is interpreted as the recent accretionary wedge.     

ScSp observed on North Island, New Zealand: implications for subducting plate structure

Seismic phase conversions provide important constraints on the layered nature of subduction zone structures. Recordings from digital stations in North Island, New Zealand, have been examined for converted ScS ‐to‐ p ( ScSp ) arrivals from deep (>150 km) Tonga–Kermadec earthquakes to image layering in the underlying Hikurangi subduction zone. Consistent P ‐wave energy prior to ScS has been identified from stations in eastern and southern North Island, where the subducted plate interface is at a depth of between 15 and 30 km. Two ScS precursors are observed. Ray tracing indicates that the initial precursor ( ScSp ₁) corresponds to conversion from the base of an 11–14 km thick subducting Pacific crust. The second precursor is interpreted as a conversion from the top of the subducting plate. The amplitude ratio, ScSp ₁: ScS , increases from 0.10 to 0.19 from northern to southern North Island. This is within the range expected from a simple first‐order velocity discontinuity at an oceanic Moho. A 1–2 km thick layer of low‐velocity sediment at the top of the subducting plate is required to explain the remaining ScSp waveform. Our results imply that the abnormally thick Hikurangi–Chatham Plateau has been subducting beneath New Zealand for at least 2.9 Myr, thus explaining the high uplift rates observed across eastern North Island.     

弹性地基上水工结构各向异性Mindlin底板计算分析的无单元法（EFGM）

无单元法（element free galerkin method）是一种基于滑动最小二乘法构造插值函数的无网格数值方法。以该方法中插值函数及其导函数为基础,从变分原理出发,建立了弹性地基上正交各向异性Mindlin板的无单元法求解控制方程,其中弹性地基采用Winkler地基模型。对该理论方法进行了相应的程序实现,最后通过算例分析表明了提出方法用于水工结构中弹性地基板问题分析的可行性和有效性。