Magnetostratigraphy of the Plio‐Pleistocene carbonate section of the Great Australian Bight

ODP Leg 182 drilled two north‐south transects in the western Great Australian Bight close to longitude 128°E. These transects penetrated a remarkably thick section of uppermost Pliocene and Pleistocene carbonate sediments, which are separated from Miocene sections by a major hiatus. In the eastern transect, at sites 1129, 1131 and 1127, the Brunhes‐Matuyama boundary (onset of C1n) was found at 343 m, between 280 and 300 m, and at 343 m below the sea floor, respectively. In the western transect, at sites 1132 and 1130, it was found between 170 and 181 m, and at 200 m, respectively. Within the Brunhes chron, inclination and intensity fluctuations and correlations between susceptibility and standard δ¹⁸O records were used to give age‐depth relations. These age relations from the palaeomagnetics are broadly consistent with the biostratigraphy and the δ¹⁸O results from Leg 182, but do not provide an entirely independent dataset. Rock magnetism stratigraphy at site 1131 revealed the principal bryozoan buildup to be at the time of the last glacial lowstand, as suggested by previous workers. At all sites the sedimentation rate increases from the basal unconformity up into the thick Upper Pleistocene section. In the western transect there appears to be a partial record of most of the Late Pliocene and Early Pleistocene chron boundaries (C1r1n to C2An3n) in a condensed section, but in the eastern transect only the Jaramillo (C1r1n) is observed.     

Geography and National Education Policy

Abstract

The National Geography Standards must be relevant to everyone associated with educational reform. The special advantage enjoyed by geography during the last administration is slipping away. The focus has shifted from the national to the local level. One way geography can demonstrate its relevance is to strengthen its ties with environmental education.     

SVD分析揭示的澳大利亚高压年际变化对中国夏季降水的可能影响

澳大利亚高压是东亚夏季风系统的重要成员之一,其对中国夏季气候存在显著影响.为了进一步弄清年际时间尺度上的澳大利亚高压变化对中国东部夏季降水的影响,利用澳大利哑海平面气压和中国夏季降水站点资料,使用SVD和线性回归方法揭示了澳大利亚高压的年际变化与中国夏季降水异常的联系,得到:SVD的第1模态的时间系数与通常使用的澳大利亚高压指数相关可达到0.98.在有无考虑ENSO的影响时,SVD的第1模态均反映出澳大利亚高压的年际变化与中国江南地区夏季降水存在密切联系,也即澳大利亚高压增强(减弱)时,江南地区降水增多(减少).澳大利亚高压对中国夏季降水的可能影响途径为:澳大利哑高压通过影响赤道纬向气流和越赤道气流并通过类似PJ波列的方式影响到中国东部地区:澳大利亚高压增强时,造成西太平洋副热带高压偏南、偏西,同时,105°E处越赤道气流显著加强,为江南地区提供充足水汽源,利于中国江南地区降水;澳大利亚高压减弱时,情况相反;在强(弱)澳大利哑高压年,印度尼西亚及热带辐合带海区SSTA负(正)异常使得低层风场的异常辐散(辐合),激发了澳大利哑南部以及西太平洋地区异常反气旋(气旋)环流,同时江南地区出现异常辐合(辐散),引起大气异常上升(下沉)运动,有利于中国江南地区夏季降水异常偏多(偏少).     

城市管理视角下的城市化问题及其解决途径

20世纪80年代以来中国的城市化进程不断加速,城市化水平达到46%,并且仍在稳步前进。如此迅速的城市化进程给城市管理带来两方面问题:一是城市发展与城市生态环境的矛盾,二是城市弱势群体的生存与城市管理秩序之间的矛盾。为缓解并消除上述矛盾,本文提出要加强城市管理的组织机构建设;加大城市规划政策协调引导力度;完善城市基础设施,提供优质的公共物品;出台多元化、有针对性的就业政策;完善社会保障体系。     

震情泄露的社会效应对策及其反思

地震震情是社会公众敏感的问题。1991年1月中旬,江苏盐城、镇江、无锡等地因震情泄露而引起强烈的社会反响。本文以镇江为例,概述了以电话潮、抢购热、防震风、保险热、谣言惑众、异常骤增为表现形式的社会效应;介绍了地方政府发挥领导指挥机能,采取富有成效的应急对策,市县地震办公室发挥政府职能作用,积极配合,迅速平息地震风波,取得显著成效;最后从行为评估、得失评估、预测预报、震情保密、社会宣传诸方面进行反思,总结经验教训,以便进一步发挥政府减灾职能作用,做好地震工作。     

Geographical Dimensions of Environmental Restructuring in New Zealand*

During the 1980s, New Zealand underwent a period of dramatic economic, social, and administrative restructuring. The reform extended to the administrative arrangements for environmental management. A geographic restructuring model is used in this paper to establish the context in which the reforms were carried out. A combination of economic, environmental, and social influences operating at different geographic scales can be identified. These influences are subsequently illustrated through reference to three aspects of the restructuring that have distinct geographical dimensions: the definition of human-environment relations, the spatial definition of planning regions, and the implications of spatial differentiation for resource management policy and practice.     

数字北京及空间信息资源建设

首都信息化的战略口号和奋斗目标是建设“数字北京” ,目的是使城市成为有利于人类生存与可持续发展的空间 ,为政府提供更加有效的、科学的管理与决策。本文主要介绍了遥感等空间信息资源在数字北京总体框架中的地位 ,以及整合并开发北京市空间信息资源达到信息共享、服务首都信息化的基本情况     

1.8–1.5-Ga links between the North and South Australian Cratons and the Early–Middle Proterozoic configuration of Australia

The Archaean and Early–Middle Proterozoic (1.8–1.5 Ga) terranes of the North Australian Craton and the South Australian Craton are separated by 400 km of ca. 1.33–1.10-Ga orogenic belts and Phanerozoic sediments. However, there is a diverse range of geological phenomena that correlate between the component terranes of the two cratons and provide evidence for a shared tectonic evolution between approximately 1.8 and 1.5 Ga. In order to honour these correlations, we propose a reconstruction in which the South Australian Craton is rotated 52° counterclockwise about a pole located at 136°E and 25°S (present-day coordinates), relative to its current position. This reconstruction aligns the ca. 1.8–1.6-Ga orogenic belts preserved in the Arunta Inlier and the Gawler Craton and the ca. 1.6–1.5-Ga orogenic belts preserved in the Mount Isa Block and the Curnamona Province. Before 1.5 Ga, the South Australian Craton was not a separate entity but part of a greater proto-Australian continent which was characterised by accretion along a southward-migrating convergent margin (ca. 1.8–1.6 Ga) followed by convergence along the eastern margin (ca. 1.6–1.5 Ga). After 1.5 Ga, the South Australian Craton broke away from the North Australian Craton only to be reattached in its current position during the ca. 1.33–1.10 Ga-Albany–Fraser and Musgrave orogenies.