《地质学报》（英文版）评选出2019年度优秀论文

《地质学报》（英文版）是中国最早的一本地学期刊,随着中国地质学会的成立而诞生,至今已走过 99 个年头,是我国最著名的地学刊物之一, 在国际上亦有很高声誉,多年来一直被 “SCI” 收录,连续8年获得中国知网等评出的“中国最具国际影响力科技期刊”称号（即依据被“SCI”统计源期刊引用数据,按一定公式计算,位居中国科技期刊的前5%）。在中国科协等“登峰计划”项目和“卓越计划”项目的支持下,中国地质学会评选了《地质学报》（英文版）2019年度优秀论文。本次评选,主要由《地质学报》（英文版）编辑部负责探索试行。为了得到文章发表后的准确的学术影响情况,本次评选的论文限于2016年第1期至2018年第6期刊出的文章。 文章形式以Article为主,兼顾少量Review; 消息报道等短文不在评选范围, 所有增刊也不参与评选。编辑部查阅了上述评选范围内各篇文稿第一作者和通讯作者的学术背景、学术能力及学术道德,文章在SCI和CNKI系统中的被引用情况,文稿投稿时的专家评审意见等内容,经综合评判,并注意兼顾不同单位和不同专业,得出初步候选文章,经主编、副主编和学会秘书长审定,最终评选出15篇文章为优秀论文。     

京津冀城市群产业空间重构与优化调控

科学解析京津冀城市群产业空间重构不仅有助于深化产业空间演化相应理论,也是服务京津冀协同发展国家战略的必然要求。论文从全球价值链视角出发,基于社会经济统计数据与全国工业企业库数据,采用经校正的产业比重变动方法对京津冀城市群产业空间重构进行了解析,并据此提出优化调控对策。主要结论有：① 产业空间重构是推动城市群发育与成熟的重要动力,其中嵌入全球价值链并持续攀升是推动城市群高级化的基础动力,而内部产业空间重构则是完善产业合作网络、推动城市群一体化的重要途径,此外,资源环境承载力与全球化、郊区化的交互是形成双“C”字形空间格局的基础与支撑;② 在国际产业空间重构方面,目前天津市为承接核心,北京次之,其余城市发展则相对滞后;③ 在城市群内部产业空间重构方面,由北京—天津—唐山—沧州围成的内“C”字形范围是产业空间重构的核心区,不同类型产业表现出不同的驱动特征,其中纺织服装业表现为全球价值链主导下的市场驱动,化学产业表现为环境管制与水资源依赖的双重作用,钢铁产业表现为明显的政府主导,医药制造业则表现为全球价值链主导下的政府调控;④ 京津冀城市群的内“C”字形地区应侧重产业升级,外“C”字形地区则重点关注生态环境保护与产业转型,以内“C”引领外“C”,以外“C”保障内“C”,双“C”联动,以保障京津冀协同发展战略的顺利实现。     

青藏高原城镇化与生态环境交互影响关系分析

科学评估青藏高原城镇化与生态环境交互影响的总体状况,对优化城镇化速度和质量,修复和提升生态环境状态具有重要意义。在梳理青藏高原城镇化与生态环境交互影响研究进展基础上,本文尝试构建一套完整的城镇化与生态环境交互影响分析模型体系,实现从综合评价指数分析、耦合协调度量化、耦合类型识别、解耦路径探索到未来趋势预测的全过程解析。以青藏高原及其省域、地级单元多尺度分析对比为手段,尝试厘清尺度之间的差异性,识别出问题区域,并提出针对性的改进措施。研究发现,青藏高原不同尺度间城镇化综合评价指数呈阶段性上升趋势,青海的整体城镇化指数高于西藏;生态环境指数变化趋势不同,青海呈下降态势,西藏则趋向平稳,各地级单元生态环境指数存在分层现象。青藏高原不同尺度城镇化与生态环境耦合协调度总体呈上升趋势,协调类型由失调衰退类向濒临失调衰退类转变,最后转为勉强协调发展类,基本属于城镇化滞后型。城镇化指数与生态环境指数呈现出强脱钩、弱脱钩交互出现的波动态势,说明不同尺度间存在城镇化与生态环境的负相互作用,消极城镇化现象突出。通过预测,青藏高原各地级单元在未来10年内,系统耦合协调度将稳步上升,但各地增长速度将存在显著差距。     

Problems and countermeasures on main mineral resource sustainable supply in northeastern China

northeastern China is an important old industrial base in China. Mineral resources are the foundation of industry development. However, because of long-term exploitation of mineral resources in northeastern China, the mineral resources reserves decrease gradually and some mineral resources are nearly exhausted, which restricts revitalization and sustainable development of the northeast old industrial base. On the basis of the comprehensive analysis of development and utilization status of mineral resources and supply and demand situation of main mineral resources in northeastern China, the authors put forward countermeasures on main mineral resources sustainable supply in northeastern China.     

A New Arthropod, Guangweicaris Luo, Fu et Hu gen. nov. from the Early Cambrian Guanshan Fauna, Kunming, China

The Guanshan Fauna is a soft-bodied fauna dominated by arthropods （including trilobites, trilobitoides, Tuzoia, Isoxys, and bradorids） in association with priapulids, brachiopods, anomalocaridids, vetulicoliids, sponges, chancellorids, and echinoderms. This paper reports and describes a new arthropod from the yellowish green mudstone at the lower part of the Wulongqing Formation, Canglangpuan Stage, Lower Cambrian in Kunming, Yunnan, China. The stratigraphic and geographic distribution, classification, fossil preservation, life style of this new arthropod and comparisons with other fossil arthropods are also discussed in details. The discovery and research of the non-mineralized arthropod, Guangweicaris Luo, Fu et Hu gen. nov. from the Guanshan Fauna adds new members to the taxonomic list and provides new information to the evolution of early arthropods. Furthermore, this study would shed new light into the ＂Cambrian Explosion＂ and the evolution of early life.     

Geochemistry and Modes of Occurrence of Hazardous Trace Elements in the No. 11 Coal Seam, Antaibao Surface Mine, Shanxi Province

Concentrations of seventeen hazardous trace elements including As, Pb, Hg, Se, Cd, Cr, Co, Mo, Mn, Ni, U, V, Th, Be, Sb, Br and Zn in the No.ll coal seam, Antaibao surface mine, Shanxi Province were determined using Instrumental Neutron Activation Analysis （INAA）, Inductively Coupled Plasma Atomic Emission Spectrometry （ICP-AES）, Cold-Vapor Atomic Absorption Spectrometry （CV-AAS） and Graphite Furnace Atomic Absorption Spectrometry （GF-AAS）. Comparisons with average concentrations of trace elements in Chinese coal show that the concentrations of Hg and Cd in the No. 11 coal seam, Antaibao surface mine are much higher. They may be harmful to the environment in the process of utilization. The variations of the trace elements contents and pyritic suffur in vertical section indicated that： （a） the concentrations of As, Pb, Mn, and pyritic sulfur decrease from roof to floor; （b） the concentrations of Cr, Zn and Mo are higher in roof, floor and lower in coal seam; （c） the concentration of Br, Sb, and Hg are higher in coal seam and lower in roof and floor; （d） the concentrations of Mo, V, Th and AI vary consistently with the ash yield. Cluster analysis of trace elements, pyritic sulfur, ash yield and major elements, such as AI, Fe, P, Ca shows that： （a） pyritic sulfur, Fe, As, Mn, Ni, Be are closely associated and reflect the influence of pyrite; （b） Mo, Se, Pb, Cr, Th, Co, Ca and A! are related to clay mineral, which is the main source of ash; （c） U, Zn, V, Na, P maybe controlled by phosphate or halite; （d） Hg, Br, Sb and Cd may be mainly organic-associated elements which fall outside the three main groups. The concentration distribution characteristics of trace elements in coal seam and the cluster analysis of major and trace elements showed that the contents of trace elements in the No. 11 coal seam, Antaibao surface mine, are mainly controlled by detrital input and migration from roof and floor.     

Metallogeny of the Lannigou Sedimentary Rock-hosted Disseminated Gold Deposit in Southwestern Guizhou Province, China

The Lannigou deposit is a large-sized sedimentary rock-hosted disseminated gold （SRHDG） deposit located in the Youjiang Basin. It is hosted by the Middle Triassic turbidite. Wall rock alterations, including silicification, pyritization, arsenopyritization, carbonatization and argillization, commonly occur along fractures. PGE study demonstrates that either Permian basalts or Triassic ultrabasic intrnsives are unlikely to be the main source of gold mineralization. Coupled with the lack of other nmgmatic activity in the vicinity of the mining area, an amagmatic origin is proposed. Organic matter compositions and GC-MS analysis of the ores and host rocks show that the organics in the ores and the host rocks have a common source; the organic matter in the ores was mainly indigenous. The positive correlation between S2 and Au contents, along with the common occurrence of organic inclusions, suggest involvement of organic matter in the ore-forming process in terms of promoting Au leaching from the source rocks, making colloidal Au migration possible, as well as hydrocarbon reduction of sulphate. Geological and geochemical characteristics of the Lannigou deposit suggest that it was formed through circulation of meteoric water and probably less importantly organic bearing formation water driven by high geothermal gradient caused by late Yanshanian extension, which leached Au from the source bed, and then migrated as Au-bisnlfides and colloidal Au, culminating in deposition by reduction-adsorption and surface complexation of gold onto the growth surface of arsenlan pyrite.     

Occurrences of Excess ^40Ar in Hydrothermal Tourmaline： Interpretations from ^40 Ar-^39Ar Dating Results by Stepwise Heating

The occurrences of excess ^40Ar within a hydrothermal tourmaline is discussed in term of the analysis data of syngenetic muscovite and tourmaline from the Lushui hydrothermal tin-tungsten deposit in western Yunnan, China, using the ^40Ar-^39Ar stepwise heating technique. About 80% excess ^40 Ar was released in the last step when the tourmaline was fused, corresponding to a release of only -3% ^39 Ar （K）, which indicates that most excess ^40 Ar was held in the mineral lattice rather than in the channels parallel to the Z-axis. This suggests that the excess ^40 Ar was incorporated during crystallization and not diffused into the tourmaline during the post-crystallization history.