Carbonate Sequence Stratigraphy of a Back-Arc Basin： A Case Study of the Qom Formation in the Kashan Area, Central Iran

The Qom Formation comprises Oligo-Miocene deposits from a marine succession distributed in the Central Basin of Iran. It is composed of five members designated as A-F. Little previous work exists on the sequence stratigraphy. Based on an integrated study of sequence stratigraphy with outcrop data, wells and regional seismic profiles, the Qom Formation is interpreted as a carbonate succession deposited in a mid-Tertiary back-arc basin. There are two second-order sequences (designated as SS1 and SS2) and five third-order sequences (designated as S1-S5). Five distinct systems tracts including transgressive, highstand, forced regressive, slope margin and lowstand have been recognized. The relationship between the sequences and lithologic sub-units has been collated and defined (S1 to S5 individually corresponding to A-C1, C2-C4, D-E, the lower and upper portions of F); a relative sea level change curve and the sequence stratigraphic framework have been established and described in detail. The coincidence of relative sea level change between that of the determined back-arc basin and the world indicates that the sedimentary cycles of the Qom Formation are mainly controlled by eustatic cycles. The variable combination of the systems tracts and special tectonic-depositional setting causally underpin multiple sequence stratigraphic framework styles seen in the carbonates of the back-arc basin revealing: (1) a continental margin basin that developed some form of barrier, characterized by the development of multiple cycles of carbonate-evaporites; (2) a flat carbonate ramp, which occurred on the southern shelf formed by the lack of clastic supply from nearby magmatic islands plus mixed siliciclastics and carbonates that occurred on the northern shelf due to a sufficient clastics supply from the land; and (3) a forced regressive stratigraphic stacking pattern that occured on the southern shelf and in basin lows due to the uplifting of the southern shelf. Thick and widespread aggradational framework limestone usually occurs in the initial sequences (S1 and S3) of the supersequence, which led to preferential oil reservoir deposition but a lack of source and cap rocks, whereas the retrogradational and progradational framework limestone usually occurs in the later sequences (S2 and S4-S5) of the supersequence, which results in two perfect sets of source, reservoir and cap rock assemblies, so that the limestone in sub-member C2-C4 and the F-Member can be predicted as important objects for oil exploration.     

哀牢山-金沙江碱性岩带南段云南金平八一村钾质碱性花岗岩锆石SHRIMP U-Pb年龄

云南省金平县八一村钾质碱性花岗岩中的锆石由岩浆锆石和岩浆复合型锆石(老核新壳锆石)组成，以后者居多。锆石定年结果表明，岩浆锆石和岩浆复合型锆石的新壳SHRIMP U-Pb年龄为37Ma，反映岩浆上侵定位时的结晶时间，相当于始新世晚期。锆石老核获得的最大年龄为510Ma和177Ma，相当于晚寒武世和中侏罗世，表明该岩体保存有寒武纪和侏罗纪地质事件信息，而42～48Ma年龄可能是混合年龄。最后对锆石的成因和花岗岩的成岩机制等进行了初步探讨。     

南海新生代构造演化及岩石圈三维结构特征

地震层析资料表明，南海地区，自红河口向南经南海、苏禄海到苏拉威西海，岩石圈速度低，底部横波速度仅4．4km／s，岩石圈厚度在60～80km之间，为薄岩石圈地区。软流层的速度也较低，在4．2-4．4km／s之间，但厚度较大，大于200km。从红河-莺歌海断裂带经南海到苏禄海，存在一条北西向宽约200km的上地幔北西向低速带，面波速度在4．05～4．25km／s之间。由上述资料可见，东亚大陆边缘及边缘海的上地幔存在一巨型低速带，在南海地区低速带的走向为北西向，在东海地区为北北西向。这种走向与地表的区域构造走向基本一致，反映这里新生代构造活动可能与地幔低速带分布有关，即上地幔低速带反映了岩石圈的区域流动。这类岩石圈区域流动引起岩石圈表层的张性构造，形成裂谷及稍后的海底扩张，在亚洲东部边缘形成一系列边缘海盆。     

Au的迁移形式及沉淀机制研究的某些进展

本文主要概述国外Ａｕ的迁移形式及沉淀机制研究的进展．Ａｕ可呈多种形式迁移,在低温热浪中,主要呈硫氢络合物或与有机质吸附在一起搬运;而在高温热液系统中,Ａｕ主要以氯络合物形式迁移。成矿流体沸腾、有机质作用、非晶态硫化物表面吸附及流体混合与围岩的相互作用等是金矿床形成的主要机理．     

Seismic Velocity Structure and Composition of the Continental Crust of Eastern China

On the basis of a one-by-one latitude-longitude grid three-dimensional seismic velocity model, the crustal P-wave velocity structure in eastern China (105-125°E and 18-41°N) is obtained, and a set of geotherms for each grid is established for P-T correction on P-wave velocities. The average depths of sub-crustal layers and their average P-wave velocities of 18 tectonic units in eastern China are exhibited. Our result presents a 32-34 km thick crust beneath eastern China, which is thinner than previous studies, with an average velocity of 6.54 km/s, corresponding to a 5 kg/m3 variation in crustal mean density. The thicker upper but thinner middle and lower crust results in a lower average seismic velocity of eastern China. An intermediate crustal composition with a SiO2 content of 59.7 wt% has been estimated. However, there exists a significant lateral variation in the crustal structures among the tectonic units of eastern China. The structure and composition features of some regions in eastern China in     

珠江三角洲及其邻近海域第四纪地质与地震危险性

从第四纪地质研究的角度分析了珠江三角洲地区的地震危险性,认为北东,近东西和北西向三组断裂带把整个珠江三角洲断陷分割成７个次一级断块,并根据控制各次级断块的断裂第四纪活动性的强弱。     

香港地区地震危险性分析

在前人研究的基础上,对香港地区的潜在震源区及有关地震活动性参数作了研究和调整。对不同学者给出的衰减关系作了对比和分析,并将计算结果与近年不同学者在邻近地区的工作成果作了比较,最后进行了不确定性分析。结果表明,香港地区５０年超越概率１０％的基岩水平加速度峰值（ＰＧＡ）界于７５ｇａｌ和１１５ｇａｌ之间,九龙场点为９２７ｇａｌ,本区各场点的地震基本烈度为Ⅶ度。     

地理信息系统在海水养殖环境研究中的应用

本文概述了目前我国海水养殖环境所面临的主要问题，分析了GIS技术及其在养殖水域生态环境研究中的功能和作用，尝试性地探讨了GIS技术的数据收集、管理和分析的强大功能在养殖水域生态环境研究中的若干应用及其发展前景，并以广东考洲洋养殖水域的环境监测作为示例加以阐述。     

International progress and evaluation on interactive coupling effects between urbanization and the eco-environment

Global urbanization is exerting severe stress and having far-reaching impacts on the eco-environment, and yet there exists a complex non-linear coupling relationship between the two. Research on the interactive coupling effect between urbanization and the eco-environment will be a popular area of study and frontier in international earth system science and sustainability science in the next 10 years, while also being a high-priority research topic of particular interest to international organizations. This paper systematically collates and summarizes the international progress made in research on interactive coupling theory, coupling relationships, coupling mechanisms, coupling laws, coupling thresholds, coupling models and coupling optimization decision support systems. The research shows that urbanization and eco-environment interactive coupling theories include the Kuznets curve theory, telecoupling theory, planetary boundaries theory, footprint family theory and urban metabolism theory; most research on interactive coupling relationships is concerned with single- element coupling relationships, such as those between urbanization and water, land, atmosphere, climate change, ecosystems and biodiversity; the majority of research on interactive coupling mechanisms and laws focuses on five research paradigms, including coupled human and nature systems, complex social-ecological systems, urban ecosystems, social-economic-natural complex ecosystems, and urbanization development and eco-environment constraint ring; the majority of interactive coupling simulations use STIRPAT models, coupling degree models, multi-agent system models and big data urban computer models; and research has been carried out on urbanization and eco-environment coupling thresholds, coercing risk and optimal decision support systems. An objective evaluation of progress in international research on interactive coupling between urbanization and the eco-environment suggests that there are six main research focal points and six areas lacking research: a lot of research exists on macroscopic coupling effects, with little research on urban agglomeration and scale coupling effects; considerable research exists on single-dimension coupling effects, with little on multiple-dimension coupling effects; a great deal exists on “one-to-one” dual- element coupling effects, with little on “many-to-many” multiple-element coupling effects; a lot exists on positive feedback coupling effects, and little on negative feedback coupling effects; a great deal exists on empirical coupling effects, and little on theoretical coupling effects; a great deal exists on the use of simple quantitative methods, and little on using integrated simulation methods. Future studies should focus on coupling effects between urbanization in urban agglomerations and the eco-environment, spatial scale coupling effects, multi-dimensional coupling effects, telecoupling effects, “one-to-many” and “many-to-many” element coupling effects, and positive and negative feedback coupling effects. There is also a need to strengthen the development and application of dynamic models for multi-element, -scale, -scenario, -module and -agent integrated spatiotemporal coupling systems and further improve theoretical innovations in coupling effect research and integrate and form complete and diverse coupling theoretical systems.     

中国城镇化发展的地理学贡献与责任使命

城镇化是中国全面建成小康社会和实现现代化的必由之路,中国城镇化不仅决定着中国的未来,而且决定着世界城镇化的进程。近35 a来中国地理学家对中国城镇化发展做出了重要贡献,主要表现在：首次提出了城镇化的概念,推动城镇化上升为国家战略;率先将Northam提出的城镇化发展三阶段论修正为四阶段论;提出了中国城镇化发展合理进程并被《国家新型城镇化规划》采用;研制了中国新型城镇化综合区划,构建了中国新型城镇化合理格局;率先研制了城镇化发展质量定量测度方法与系统,为提升城镇化发展质量提供了技术支撑;较早发布了《中国新型城镇化发展报告》,提出了新型城镇化发展的通用模式和差异模式;首次提出了城镇化与生态环境耦合圈理论与技术图谱。中国地理学家在城镇化这一多学科研究的重大领域中经常扮演着组织者角色,并担当重任,主要是：综合分析城镇化发展面临的问题及国际经验,探索城镇化发展的驱动机制与基本规律,辨析城镇化发展的空间格局和差异模式,揭示城镇化发展与资源环境的耦合关系,模拟预警城镇化发展的多种情景与风险,选择城镇化发展质量提升的可持续之路。今后一段时间内,创新国家新型城镇化高质量发展理论,优化“一带一路”背景下中国城镇化发展的空间格局,揭示中国城镇化与生态环境交互耦合机理及规律,研制中国城镇化发展的智能决策支持系统与引导政策,是中国城镇化发展的地理学使命。