福建省地体构造划分及构造演化

本文根据对福建省不同地区的地质特征进行详细的研究对比,划分出闽西北、闽西南、闽东和闽东南四个性质不同的地体,并研究了各地体的之间碰撞拼贴的历史,指出它们主要经历了三个阶段：1、晚元古代,闽西南地体和闽西北地体沿南平-宁化一线发生碰撞拼贴作用,同时伴随海底和陆上火山喷发活动;2、三叠纪,闽东地体沿政和-大埔一线和闽西南、闽西北地体发生碰撞拼贴作用,闽东南地体也随之拼贴在闽东地体之上;3、白垩纪,闽东南地体沿平潭一东山断裂带发生左行走滑运动。     

Tectonic Evolution of an Early Precambrian High-Pressure Granulite Belt in the North China Craton

A large-scale high-pressure granulite belt (HPGB), more than 700 km long, is recognized within the metamorphic basement of the North China craton. In the regional tectonic framework, the Hengshan-Chengde HPGB is located in the central collision belt between the western block and eastern block, and represents the deep crustal structural level. The typical high-pressure granulite (HPG) outcrops are distributed in the Hengshan and Chengde areas. HPGs commonly occur as mafic xenoliths within ductile shear zones, and underwent multipile deformations. To the south, the Hengshan-Chengde HPGB is juxtaposed with the Wutai greenstone belt by several strike-slip shear zones. Preliminary isotopic age dating indicates that HPGs from North China were mainly generated at the end of the Neoarchaean, assocaited with tectonic assembly of the western and eastern blocks.     

A quantitative research for present-time crustal motion in Fujian Province, China and its marginal sea

Based on the Chinese mainland GPS network (1994～1996), Fujian GPS network (1995～1997), cross fault deformation network (1982～1998), precise leveling network (1973～1980) and focal mechanism solutions of the recent several tens years, we synthetically and quantitatively studied the present-time crustal motion of the southeast coast of Chinese mainland-Fujian and its marginal sea. We find that this area with its mainland together moves toward SE with a rather constant velocity of 11.2(3.0 mm/a. At the same time, there is a motion from the Quanzhou bay pointing to hinterland, with a major orientation of NW, extending toward two sides, and with an average velocity of 3.0(2.6 mm/a. The faults orienting NE show compressing motions, and the ones orienting NW show extending motions. The present-time strain field derived from crustal deformation is consistent with seismic stress field derived from the focal mechanism solutions and the tectonic stress field derived from geology data. The principal stress of compression orients NW (NWW) - SE (SEE). Demarcated by the NW orienting faults of the Quanzhou bay and Jinjiang-Yongan, the crustal motions show regional characteristics: the southwest of Fujian and the boundary of Fujian and Guangdong are areas of rising, the northeast of Fujian are areas of sinking. The horizontal strain rate and the fault motion of the former are both greater than the later. The side-transferring motion of Hymalaya collision zone and the compression of the west pacific subduction zone affect the motion of the research area. The amount of motion affected by the former is larger than the later, but the former is homogeneous and the later is not, which indicates that the events of strong earthquakes in this region relate more directly with western pacific subduction zone.     

腾冲火山活动构造动力学研究

利用腾冲火山区域 (10°～ 35°N ,90°～ 10 6°E) 1990～ 1998年 6 6 0个地震基本参数和震源机制资料 ,以及原先已作过 370多个强震震源参数资料[1 ] ,并结合本区域的地质资料 ,对本区的火山作用的构造动力学以及腾冲火山与印度、欧亚两大板块的关系作了探讨。研究表明 ,腾冲火山区西侧的印度板块对缅甸板块和包括腾冲在内的滇缅泰板块作用 ,大致在 0～ 10 0km作用机制表现为斜俯冲 ,10 0km以下表现为碰撞挤压作用。分析还表明 ,腾冲火山的形成与活动 ,与印度板块和亚欧板块两个大陆板块俯冲、碰撞 ,及在缅甸那加山、阿拉干山板块缝合线产生的斜俯冲和侧面挤压剪切作用密切相关 ,它应该属于两个大陆板块碰撞型板缘火山。     

Seismological Evidences for the Multiple Incomplete Crustal Subductions in Himalaya and Southern Tibet

SEISMOLOGICAL EVIDENCES FOR THE MULTIPLE INCOMPLETE CRUSTAL SUBDUCTIONS IN HIMALAYA AND SOUTHERN TIBET     

Triple collisions in the one-dimensional three-body problem

We consider the motions of particles in the one-dimensional Newtonian three-body problem as a function of initial values. Using a mapping of orbits to symbol sequences we locate the initial values leading to triple collisions. These turn out to form curves which give clear structure to the region in which the motions depend sensitively on initial conditions. In addition to finding the triple collision orbits we also locate orbits which end up to a triple collision in both directions of time, that is, orbits which are finite both in space and time. This revised version was published online in July 2006 with corrections to the Cover Date.     

高原大桥桥台地震破坏机理与抗震措施分析

通过现场震害调查和有限元分析,研究了汶川大地震高原大桥桥台的地震破坏机理和提高桥台抗主梁撞击能力的工程措施。研究表明,基于pushover静力分析技术可较好地模拟桥台在主梁撞击下的破坏形态。对不同的有限元模型假定,高原大桥虹口侧桥台可表现出"上弱下强"、"上下等强"和"下弱上强"等3种不同的破坏模式,且桥台胸墙、前墙、前墙与翼墙交界面是抗震薄弱点,在主梁撞击下易发生脆性开裂;而高原侧桥台的破坏则基本为自胸墙开始,沿45°夹角向斜下方扩展,最终导致桥台胸墙撞碎、后侧翼墙脱落倒塌。素混凝土桥台在主梁撞击下表现出明显的脆性,提高桥台混凝土强度可有效增大桥台抗撞击的强度,而在桥台混凝土中配置一定量的分布钢筋则可有效延缓桥台破坏过程。     

Relaxation method for pounding action between adjacent buildings at expansion joint

Earthquake‐induced structural pounding frequently causes serious damage to buildings, particularly at the expansion joint (hereafter, EXPJ) between adjacent buildings. Because the EXPJ width in existing reinforced concrete buildings is usually very small, typically about 5 cm for school buildings in Japan, collision avoidance cannot be achieved by seismic retrofitting. This paper presents an experimental investigation into an effective method for reducing severe structural damage due to pounding at the EXPJ between narrowly separated buildings. The method involves inserting a shock‐absorbing material such as rubber into the EXPJ gap. The efficiency of the proposed method is evaluated by laboratory shaking tests using two model buildings. Furthermore, a lumped mass model is used to carry out a collision analysis in order to numerically investigate the influence of such a shock‐absorbing material. Both the numerical and experimental results confirm the effectiveness of the proposed approach. The validity of the proposed method is also demonstrated by numerical simulation of adjacent 10‐story steel buildings with an EXPJ width of 5 cm. The force, acceleration and velocity produced by earthquake‐induced structural pounding are found to be remarkably mitigated by inserting a soft shock‐absorbing material into the EXPJ gap. Copyright © 2014 John Wiley & Sons, Ltd.     

兴海地区中高压混杂岩片的发现及其构造意义

分布于昆秦接合部—苦海—赛什塘构造混杂带中的混杂岩片,经历了中高压绿片岩相变质和同期强烈的韧性剪切变形,经推算其变质条件P=0.5～0.7GPa,T=400～450℃,地热梯度为16～22℃/Km,属不典型的中高压变质作用产物。经研究确定,物质沉积混杂的时代为P_1—P_2,变质变形作用时间为263～278Ma,经历最后一次变质并折返时间为220～279Ma,三个时期分别代表着本区经历的古特提斯洋壳俯冲、弧陆碰撞—陆内碰撞和陆内造山作用阶段。     

BOLTZMANN方程与碰撞矩阵元的计算

作者用Ｂｕｒｎｅｔｔ函数作为展开基底表示分子速度分布函数和Ｂｏｌｔｚｍａｎｎ方程，并由此证明，Ｂｏｌｔｚｍａｎｎ碰撞矩阵元的计算归结为约化积分、Ｃｌｅｂｓｃｈ－Ｇｏｒｄａｎ系数和Ｂｒｏｄｙ－Ｍｏｓｈｉｎｓｋｙ系数的计算。为了提高计算效率，作者将这些系数用超几何函数予以表示，并由此提出了高效的计算方法。