中沙群岛近海表层沉积物中的火山灰及其对构造环境的响应

南海中沙近海表层沉积物的轻组分(粒径为63~125μm)中主要包括有褐色火山玻璃、无色火山玻璃以及火山渣等3种火山灰类型。在硅碱图(TAS)及Al2O3、FeO*、MgO、CaO、Na2O、K2O对SiO2的变化趋势图中可以判断,本区可能存在双峰式火山活动,褐色火山玻璃代表中-基性端元,而无色火山玻璃代表酸性端元。无色火山玻璃与褐色火山玻璃具有共同的岩浆源区,结晶分异可能是源区岩浆演化的主要方式。这种双峰式火山活动暗示火山活动源区处于大陆拉张减薄环境,支持西沙海槽是一个正在活化的伸展大地构造现象这一观点,同时肯定基于地球物理学和岩石学研究资料所提出的海南地幔柱的存在。     

Ultimate Strength Analysis of Offshore Jacket Platform

- The ultimate strength analysis of offshore jacket platforms is a research project which has been developed in recent years. With the rapid development of marine oil industry, the departments of design and IMR (Inspection, Maintenance and Repair) in the offshore engineering have attached great importance to this project. The research procedure applies to both the stress check of new design platforms and the whole safety assessment of existing platforms. In this paper, we combine the pseudo non-linear technique with the linear analysis program and successfully analyze the ultimate strength of the space frame structure subject to the concentrated load and a real jacket platform subject to the dead load and environmental load.     

台湾海峡沉积盆地的演化与油气远景

台湾海峡沉积盆地新生代以来构造演化经历了早第三纪陆缘裂谷、晚第三纪挤压收缩和第四纪隆起封闭等发育阶段，属残留陆缘裂谷，具有良好的油气远景，其中，海峡中部油气远景最佳。     

Metamorphic inheritance of Rheic passive margin evolution and its early‐Variscan overprint in the Teplá‐Barrandian Unit,Bohemian Massif

Rift‐related regional metamorphism of passive margins is usually difficult to observe on the surface, mainly due to its strong metamorphic overprint during the subsequent orogenic processes that cause its exposure. However, recognition of such a pre‐orogenic evolution is achievable by careful characterization of the polyphase tectono‐metamorphic record of the orogenic upper plate. A multidisciplinary approach, involving metamorphic petrology, P–T modelling, structural geology and in situ U‐Pb monazite geochronology using laser‐ablation split‐stream inductively coupled plasma mass spectrometry, was applied to unravel the polyphase tectono‐metamorphic record of metapelites at the western margin of the Teplá‐Barrandian domain in the Bohemian Massif. The study resulted in discovery of three tectono‐metamorphic events. The oldest event M1 is LP–HT regional metamorphism with a geothermal gradient between 30 and 50 °C km^?1, peak temperatures up to 650 °C and of Cambro‐Ordovician age (c. 485 Ma). The M1 event was followed by M2‐D2, which is characterized by a Barrovian sequence of minerals from biotite to kyanite and a geothermal gradient of 20–25 °C km^?1. D2‐M2 is associated with a vertical fabric S2 and was dated as Devonian (c. 375 Ma). Finally, the vertical fabric S2 was overprinted by a D3‐M3 event that formed sillimanite to chlorite bearing gently inclined fabric S3 also of Devonian age. The high geothermal gradient of the M1 event can be explained as the result of an extensional, rift‐related tectonic setting. In addition, restoration of the deep architecture and polarity of the extended domain before the Devonian history – together with the supracrustal sedimentary and magmatic record – lead us to propose a model for formation of an Ordovician passive continental margin. The subsequent Devonian evolution is interpreted as horizontal shortening of the passive margin at the beginning of Variscan convergence, followed by detachment‐accommodated exhumation of lower‐crustal rocks. Both Devonian shortening and detachment occurred in the upper plate of a Devonian subduction zone. The tectonic evolution presented in this article modifies previous models of the tectonic history of the western margin of the Teplá‐Barrandian domain, and also put constraints on the evolution of the southern margin of the Rheic ocean from the passive margin formation to the early phases of Variscan orogeny.     

四川盆地中南部地区中三叠统雷口坡组沉积相研究

川中南部地区中三叠统雷口坡组划分为3个相（开阔台地相、局限台地相、蒸发台地相）、4个亚相（潮下、泻湖、潮阃坪、潮上坪）和17个微相。沉积相横向上总体变化不大，岩性较统一，蒸发岩较发育，纵向上沉积相变化具有同步性。利用单因素法和优势相法，并结合层序地层学研究成果，把雷口坡组分为7个作图单元，较精确地展示了雷口坡纽不同层段的沉积相展布和演化。研究区内雷口坡期的相对海平面升降变化和台地次级洼隆相间的古地貌共同控制着沉积相带展布和演化。雷口坡组以局限台地相为主，主要发育在雷一段1亚段的台内滩微相，为储集体有利的发育相带，多发育于潮间高处与泻湖的过渡区附近相对高能带。     

"数字衡阳"市县一体化大数据与地理信息公共服务云平台建设的技术创新

“数字衡阳”市县一体化大数据与地理信息公共服务云平台建设项目，实现了市县地理信息一体化管理、共享和协同服务，制定了完整的市县一体化标准体系，创新了基础地理信息数据生产和管理机制，创建了基于标准体系的“一键成图”技术。大幅提升了地理信息共享应用的效益，降低了县级地理信息应用技术门槛，为全国其他地区数字城市建设提供了可借鉴、推广的经验。今后将进一步实现数据成果在各行各业的快速应用，产生更好的经济效益和社会效益。     

新时代测绘地理信息服务于自然资源统一确权登记的探索 ——以北京市自然资源统一确权登记为例

新时代，自然资源已成为支撑生态文明建设的重要基础，是建设自然资源产权制度的重要内容，也是测绘地理信息服务社会管理与经济建设的新领域。本文从测绘地理信息服务角度，立足自然资源数据采集、技术流程优化、综合信息平台搭建等多个阶段，探讨了测绘地理信息技术在自然资源统一确权登记中的技术支撑作用。     

Evaluation method for Green jack-up drilling platform design scheme based on improved grey correlation analysis

This paper presents an evaluation method for green jack-up drilling platform(GJDP) design scheme based on the improved grey correlation analysis(IGCA). Under the situation of the low-carbon economy it is important and complicated for jack-up drilling platform design to select the optimum design scheme from the feasible schemes. In this paper, the evaluation index system for GJDP has been proposed which includes 3 factors: advanced technology, economic feasibility and environmental coordination, as well as 13 sub-indices. At the same time, a multi-objective combinatorial optimization model is established by using IGCA, in which the analysis hierarchy process (AHP) is used to obtain the weight values of the indices. The IGCA method is fully considered the connection of the indices reflecting the objective true nature of the things, and the subjective interest of the platform owner and the needs of the designer. This research can not only conduct to green design of jack-up drilling platform, but also can contribute to the development, popularization and application of low-carbon technology on offshore platform. Finally, the case study results demonstrate the feasibility and efficiency of the proposed evaluation method.     

Speculative petroleum systems of the southern Pelotas Basin,offshore Uruguay

The Pelotas Basin of Brazil and Uruguay represents a frontier basin with under-explored hydrocarbon potential. Although oil and gas accumulations have yet to be identified, only 21 exploratory wells have been drilled in an area of more than 330,000 km², 20 of which are located in the Brazilian portion of the basin. A detailed study of the petroleum system of offshore Uruguay has strong potential to contribute to a better characterization of the capacity of the basin to generate and accumulate hydrocarbons. Three stages have previously been recognized during the evolution of Pelotas basin: (1) a prerift phase which preserved Paleozoic and Mesozoic units of the Paraná Basin; (2) an Early Cretaceous volcano-sedimentary synrift phase; and (3) a Cretaceous to Cenozoic postrift phase deposited during the passive margin stage. In this study, we use sequence stratigraphy methodology to interpret 2D multichannel seismic sections of the southern segment of the Pelotas Basin in the Uruguayan Atlantic margin. This analysis allows us to identify depositional sequences, systems tracts and the distribution of the main elements of the potential petroleum systems. Following our analysis, we propose six speculative petroleum systems (SPS) in the Pelotas Basin. The first SPS is related to the prerift phase and is represented by a Lower Permian restricted marine source rock and reservoirs related to Permian to Upper Jurassic aeolian and fluvial sandstones. The second SPS corresponds to the synrift phase and is constituted by a Barremian lacustrine source rock with reservoirs of alluvial/fluvial sandstones of the same age. The other four proposed SPS are associated with the postrift phase, represented by marine source rocks related to Aptian-Albian, Cenomanian-Turonian and Paleocene transgressions, all of which are identified in the region and interpreted in seismic lines from Uruguay. These postrift SPS have predominantly siliciclastic reservoirs represented by Early Cretaceous aeolian sandstones and Cretaceous to Cenozoic deltaic sandstones and turbidites.     

系缆式剖面测量平台运动性能分析

文章简单介绍了系缆式剖面测量平台的结构构成,围绕剖面测量平台升降运动的工作原理,着重对平台的一些固有的基本特性所产生的影响进行了分析,供有关人员参考交流。