陆相二叠系-三叠系界线研究进展

着重介绍了几个目前陆相二叠系—三叠系界线（TPTB）研究的重点剖面及其生物地层学研究进展；分析了陆相二叠系—三叠系界线综合地层学研究现状，包括生物地层学、事件地层学、同位素年代学、磁性地层学和层序地层学等；剖析了陆相二叠系-三叠系界线地层学研究中存在的问题及进一步的研究方向。生物地层方面，陆相二叠系-三叠系界线附近存在晚二叠世与早三叠世生物混生的层位，其中不同类别生物的时间界线常不一致，又由于陆相界线地层中含脊椎动物化石的层位一般较少，以脊椎动物化石（Lystrosaurus）为标准的精确界线常不确定，因而需重新寻找并确定陆相三叠系底界的标准化石。事件地层标志可能会成为连结海、陆相二叠系-三叠系界线地层高精度对比的纽带。     

粤港澳大湾区背景下的珠三角城市群产业—人口—空间交互影响机理

在粤港澳大湾区成为国家战略的背景下,具有经济地理优势的“湾区”地带,因作为推动全球经济发展的重要增长极而举世瞩目。本文以其主要组成部分的“珠三角9市”为研究对象,通过建立向量自回归VAR模型,利用脉冲响应函数和方差分解方法,对该城市群发展进程中的“产业—人口—空间”交互影响机理进行分析。研究结果表明：珠三角城市群的产业发展对人口的吸纳作用在后期近乎消退,人口集聚对产业发展的促进作用在中后期也明显减弱,而空间扩展对人口集聚的影响效果比较有限且后期呈现负影响。基于上述结论可以判断,珠三角城市群产业、人口和空间要素之间具有短期间的互促发展效果,但是尚未形成城市群应具有的长期稳定的互促机制。为推进粤港澳大湾区建设,珠三角城市群应积极推动产业类型不断提升以集聚高素质人口,积极引导空间扩张与人口增长匹配发展,并构筑多层次且协同互补的产业空间,以此深化产业、人口和空间要素的协同发展格局。     

粤港澳大湾区发展的理论框架与发展战略探究

粤港澳大湾区是在“一带一路”倡议下,由珠三角经济圈的强化合作而产生的新地理概念。作为新兴的全球化港湾,粤港澳大湾区如何突破新自由主义框架理论,探索出符合社会主义市场经济体制的发展路径,是当前决策者和规划者需要思考的重要问题。本文简要梳理了现有的城市群、区域增长极理论,新经济地理集群理论,全球产业链网络理论并结合大湾区现状优势,对湾区发展战略定位与发展路径进行探究,认为可通过粤港澳三方通力合作,创造一个内生型的经济与产业本土增长模式为主要方向。具体表现为：首先,要以先进制造业为立足点、实现自我创新的产业升级,形成完善的制造业产业链,并成为全球生产网络的重要节点与区域性枢纽;其次,大湾区还应利用自身的科研与教育、金融与创新资源优势,推进“一国两制三关税区”、尤其是与香港在大湾区建设中的全方位参与联动,完善产权制度,加强合规和规则经济的市场经济体系建设,将大湾区打造为中国的科创中心及全球性金融中心。     

从巨型城市区域视角审视粤港澳大湾区空间结构

粤港澳大湾区是全球高度城市化地区之一。本文引介巨型城市区域理论来审视粤港澳大湾区的空间结构发展,从边界、功能、核心区、区域基础设施4个维度进行分析。未来粤港澳大湾区将呈现四大发展趋势：一是去边界化趋势显著,大湾区内部边界地区将快速发展;二是产业区将成为网络化的功能区块,并取代城市成为地区参与全球竞争的基本单元;三是广佛、港深两大核心区将形成;四是轨道公交化趋势,大湾区共享交通枢纽与公服设施。按发展趋势预测,未来粤港澳大湾区空间结构将形成“两核+若干功能区”的新格局。     

燕山地区喜马拉雅期地壳运动划分及表现特征

摘要：在全面总结燕山地区新生代沉积相和厚度分析、地貌类型及特征、新生代岩浆活动、活动构造类型及特征、延（庆）涿（鹿）地堑盆地及其构造演化、地震地质分析以及大量的同位素年龄测试结果基础上,结合前人对邻区地壳运动划分的意见,系统地将燕山地区喜马拉雅期地壳运动划分为两期、三幕和三亚幕,为我国东部地区建立了一个比较完整的新生代地壳运动年表。     

地震序列研究综述

有关地震序列的研究大体可分三类：序列类型判别研究、序列生成机理研究、通过研究序鲁的进空图象及震源机制变化推断地下构造特征的研究等。关于序列类型判别研究,ｈ值判别法应用最广。序列生成机理的研究已有许多模型,一般认为介质结构或应力分布的非均匀性是形成序列的重要因素。但目前研究所能解释的地震序列特征还是有限的。尚无一个能较全面地解释各典型序列特征（时间－空间分布图象及强度特征等）的合理生成机理模型。精确     

The first tephra evidence for a Late Glacial explosive volcanic eruption in the Arxan-Chaihe volcanic field (ACVF), northeast China

A 5 mm thick tephra layer has been identified in the lacustrine sediments of Moon Lake in the Arxan-Chaihe volcanic field (ACVF) in Greater Khingan Mountains (NE China). The visible tephra layer is clearly revealed as a distinct peak in magnetic susceptibility measurements. The tephra layer consists mainly of brown vesicular glass shards and minor amounts of plagioclase, olivine and clinopyroxene. Major and minor element analysis has been carried out on the glass shards and plagioclase minerals. Glass shards show low concentrations of K₂O, similar to the eruptive products derived from post-Miocene volcanoes of the ACVF. The plagioclase phenocrysts in both lava and tephra from ACVF, and in the tephra recorded in Moon Lake are labradorites. During the Late Pleistocene to Holocene, there were also extensive explosive eruptions in the nearby Nuominhe volcanic field (NVF). Volcanic rocks from the ACVF are easily distinguished from those derived from the NVF, having distinctly different K₂O concentrations. This compositional variation is likely the result of different magmatic processes operating in the ACVF and NVF. Radiocarbon dating on organic materials from the lacustrine sediments dates the tephra layer to ca. 14,200 cal yrs BP, which implies that it was generated by a previously unknown Late Pleistocene explosive eruption in the ACVF. These results, for the first time, give a direct tephra record in this area, and suggest that identification of further tephra and/or cryptotephra in local sedimentary basins such as crater lakes of scoria cones and maars will be significant for dating the Late Pleistocene to Holocene volcanic eruptions and will help to establish a detailed record of the volcanic activity in the ACVF. The newly discovered tephra layer also provides a dated tephrochronological marker layer, which will in future studies provide a means to synchronise local sedimentary records of the climatically variable Late Glacial.     

2017年8月8日九寨沟MS7.0地震序列分析

2017年8月8日四川九寨沟发生M_S7.0地震,该地震发生在巴颜喀喇块体的东北边界,震中区域构造条件复杂,是巴颜喀喇块体北侧左旋走滑环境向东侧逆冲挤压环境过渡的位置,附近地区历史强震较多。九寨沟地震是一次主-余型地震,余震活动水平较弱,主震发生后短时间内M_L≥4.0余震的“等待时间”存在异常,震后较长时间余震活动恢复到正常状态,序列h值、余震视应力等符合主-余型序列特征。序列b值为0.84,G-R关系推测序列最大余震的震级约为M_L5.4（M_S5.0）,8月9日发生的M_S4.8地震是目前该序列的最强余震。通过与1970年以来附近地区7级左右地震序列的对比认为,九寨沟地震与1976年松潘-平武2次7.2级地震序列在余震空间位置、发震构造和震源机制等方面存在较大差异,因此,不具备发育为震群型序列的条件。九寨沟地震主震视应力为0.36～0.38MPa,属于应力下调模型,序列余震的平均视应力水平接近龙门山断裂带附近中小地震的平均背景水平。     

Sequence stratigraphic framework and sedimentary model of Shanxi Formation in northeast Zhoukou Depression of the North China Plate

The sequence stratigraphic framework of Shanxi Formation in the northeast Zhoukou Depression was established based on detailed sequence stratigraphical and sedimentological analysis by utilizing the logging and core data of six wells drilled in the eastern tectonic unit of Zhoukou Depression. It was divided into three third-order sequences, namely SQs1, SQs2, and SQs3 from bottom to top. Each sequence can be divided into a transgressive system tract (TST) and a highstand system tract (HST). Furthermore, four sequence boundaries and three maximum flooding surfaces were identified, and they are the bottom interface SBs and maximum flooding surface mfss1 of SQs1, the bottom interface SBs1 and maximum flooding surface mfss2 of SQs2, the bottom interface SBs3 and maximum flooding surface mfss3 of SQs3, and the top interface SBx from bottom to top. Carbonate tidal flat –clastic tidal flat sedimentary system developed in Shanxi Formation in the northeast Zhoukou Depression (also referred to as the study area) under the control of regression. Meanwhile, four sedimentary microfacies were identified in the sedimentary system, which are lime-mud flats, sand flats, mixed flats, and mud flats. The transgression in the study area occurred from the southeast to the northwest. Therefore, the northwestern part is the seaward side, and the southeastern part is the landward side. As revealed by relevant drilling data, SQs1 of the Shanxi Formation is characterized by the development of limestone and carbonaceous mudstone, with limestone, dark mudstone, and carbonaceous mudstone mainly developing. Meanwhile, lime-mud flats were mainly deposited in it. During the periods of SQs2 and SQs3, the sedimentary environment of the study area changed from the carbonate tidal flats to clastic tidal flats as the coastline migrated towards the sea. In these periods, sand flats mainly developed near the maximum flooding surfaces and were relatively continuous in the eastern and southern parts of the transgressive system tract; mixed flats were relatively continuous in the western and northern parts of the transgressive system tract as well as the eastern and southern parts of the highstand system tract; mud flats widely developed in the highstand system tract. Peat flats mainly developed in the period of HSTs2, with coal seams relatively developing in the southeastern part of the study area as revealed by drilling data. The peat flats in SQs2 are favorable hydrocarbon source layers, the lime-mud flats in SQs1 and sand flats formed in the transgression periods of SQs2 and SQs3 constitute favorable hydrocarbon reservoirs, and the mud flats form in the transgressions periods serve as favorable cap rocks. Therefore, the study area features a reservoir-cap assemblage for self-generating and self-storing of hydrocarbon, and the southeastern part of the study area can be taken as a favorable exploration area.     

2020年1月19日新疆伽师MS6.4地震序列特征及后续趋势分析

介绍2020年1月18日新疆伽师M S5.4和1月19日M S6.4两次地震的基本参数、震源机制解、精定位等资料,分析伽师M S6.4地震序列类型、序列衰减特征和余震序列各项数字地震学资料,并就该序列与历史地震序列进行对比,提出震后趋势判定意见。分析认为,该序列为前—主—余型,余震序列衰减较为迅速。