自然延伸概念及相关地质要素在海域划界中的影响效力分析

The United Nations Convention on the Law of the Sea entitled the coastal States to naturally extend the continental shelf, which has caused more drastic disputes of maritime delimitation. This paper devotes to clarifying the significant concept of natural prolongation through an effect method combing the legal principles and technical analysis. Firstly, the classic samples with respect of the development of geological features are traced. Based on these samples, the classification with a model is proposed in order to affirm the concept''s significance under certain geomorphologic situations. Lastly, scientific analysis is used to present two potential prolongation situations and emphasize that all the technical analysis on maritime delimitation should be complied with international law and protect the common interest of all the mankind.     

菲律宾蛤仔苗种土池中间培育及越冬生产实验

利用2．6hm^2和3．13hm^2 2个养虾池,经过池底清淤、底质改良、敌害清除、培养用水处理、繁殖基础饵料生物等工作后,分别移入在室内培育的菲律宾蛤仔（Ruditapes philippinarum（Adams et Reeve））壳顶后期幼虫和双水管稚贝各80亿粒和9．7亿粒,经土池中间培育、越冬后,生产出2000-3000粒／500g幼贝7．9亿粒。自移入幼虫和稚贝到幼苗出池,成活率分别为4．5％和44．3％,达到了较高水平的中间培育、越冬成活率。     

青藏高原生态地质环境遥感调查研究

自2003年始开展的青藏高原生态地质环境遥感调查与监测项目已取得了阶段性的成果，本文就项目涉及到的第四纪基础地质 与第四纪冰川遗迹、现代冰川雪线、湖泊湿地、荒漠化等专题成果进行了简要介绍。本文明确了项目开展的意义，给出了青藏高原 生态地质环境质量的评价结果，强调了地学因素对于青藏高原生态地质环境形成与演化的控制作用，以及近30a来全球气候变化对 高原生态地质环境适应性变化的驱动作用。     

Ore-forming Fluid and Mineral Source of the Hongshi Copper Deposit in the Kalatage Area, East Tianshan, Xinjiang, NW China

The Hongshi copper deposit is located in the middle of the Kalatage ore district in the northern segment of the Dananhu-Tousuquan island-arc belt in East Tianshan, Xinjiang, NW China. This study analyses the fluid inclusions and H, O, and S stable isotopic compositions of the deposit. The fluid-inclusion data indicate that aqueous fluid inclusions were trapped in chalcopyrite-bearing quartz veins in the gangue minerals. The homogenization temperatures range from 108°C to 299°C, and the salinities range from 0.5% to 11.8%, indicating medium to low temperatures and salinities. The trapping pressures range from 34.5 MPa to 56.8 MPa. The δ18OH2O values and δD values of the fluid range from ?6.94‰ to ?5.33‰ and from ?95.31‰ to ?48.20‰, respectively. The H and O isotopic data indicate that the ore-forming fluid derived from a mix of magmatic water and meteoric water and that meteoric water played a significant role. The S isotopic composition of pyrite ranges from 1.9‰ to 5.2‰, with an average value of 3.1‰, and the S isotopic composition of chalcopyrite ranges from ?0.9‰ to 4‰, with an average value of 1.36‰, implying that the S in the ore-forming materials was derived from the mantle. The introduction of meteoric water decreased the temperature, volatile content, and pressure, resulting in immiscibility. These factors may have been the major causes of the mineralization of the Hongshi copper deposit. Based on all the geologic and fluid characteristics, we conclude that the Hongshi copper deposit is an epithermal deposit.     

一次强飑线过程极端大风的中尺度分析

利用常规气象观测资料、区域自动气象站加密观测资料和GFS 0.25°×0.25°逐6 h的分析场数据以及多普勒雷达、风廓线等资料,通过背景形势场分析、物理量诊断分析和中尺度分析,对2018年3月4日发生在华东地区的强飑线天气过程进行了诊断分析。结果表明,这次过程具有发生时间(季节)早、移速快、范围广、致灾强等特点,是一次比较少见的早春(冬末)十分强烈的飑线天气过程,是在高空急流辐散区、低空西南急流轴前端、低涡南侧的暖区中发展起来的。飑线过程的地面要素变化十分剧烈,地面有强冷池,与飑线前暖空气之间构成了强的水平温度梯度,致使飑线强度更强;飑线经过时气压涌升所形成的雷暴高压、强气压梯度以及飑线的快速移动均有利于地面极端大风的出现。飑线发展过程中观测到弓形回波、超级单体等强天气系统。中高层动量下传和光滑湖面、喇叭口、狭管效应等特殊地形对于大风的增强效应比较显著,这些因素也加剧了地面极端大风的形成。      

A new approach to measurement of regional inequality in particular directions

Regional inequality is a core issue in geography,and it can be measured by several approaches and indexes.However,the global inequality measures can not reflect regional characteristics in terms of spatiality and non-mobility,as well as correctly explore regional inequality in particular directions.Although conventional between-group inequality indexes can measure the inequality in particular directions,they can not reflect the reversals of regional patterns and changes of within-group patterns.Therefore,we set forth a new approach to measure regional inequality in particular directions,which is applicable to geographic field.Based on grouping,we established a new index to measure regional inequality in particular directions named Particular Direction Inequality index(PDI index),which is comprised of between-group inequality of all data and between-group average gap.It can reflect regional spatiality and non-mobility,judge the main direction of regional inequality,and capture the changes and reversals of regional patterns.We used the PDI index to measure the changes of regional inequality from 1952 to 2009 in China.The results show that:1) the main direction of China’s regional inequality was between coastal areas and inland areas;the increasing extent of inequality between coastal areas and inland areas was higher than the global inequality;2) the PDI index can measure the between-region average gap,and is more sensitive to evolution of within-region patterns;3) the inequality between the northern China and the southern China has been decreasing from 1952 to 2009 and was reversed in 1994 and 1995.     

下扬子复杂构造区超高压含气层的发现及油气富集关键要素

下扬子地区的构造复杂性使该地区油气勘探存在极大的难度和风险,如何在复杂构造区取得油气勘探突破是近年关注的焦点。2019年皖为页1井在下扬子无为凹陷三叠系周冲村组首次发现2套异常高压含天然气层,最高地层压力系数达1.9,取得下扬子油气调查的重大突破性进展,为下扬子油气勘探困局打开了一扇窗口。基于该超压含气层的新发现,综合研究表明,无为凹陷天然气富存得益于4个关键控制要素的有机组合：①深层稳定基底;②对冲过渡带原地体;③深水裂陷黑色页岩有利相带;④多套膏盐有利封盖等。为无为凹陷提供了稳定构造背景、良好构造保存、有利烃源岩及优质盖层等条件。上述地质要素同样有利于该凹陷二叠系页岩气富集,由此提出了构造复杂区三叠系常规天然气与二叠系页岩气一井双探的新思路。上述关键4个要素在下扬子区域上的配置关系显示,望江凹陷与无为凹陷具有相似的地质条件,是下一步油气勘探的首选有利区。     

新疆晚古生代大陆边缘成矿系统与成矿区带初步探讨

新疆地处中亚成矿域的中段,古生代大陆边缘增生明显、构造和岩浆活动强烈、矿产资源丰富。古生代大陆边缘成矿作用主要集中在两个时期,即以阿尔泰南缘为主的早中泥盆世和以天山为主的早石炭世。本文在综合研究及与境外对比的基础上,按照北疆地区晚古生代大陆边缘的构造动力学和成矿特征,将研究区大陆边缘成矿系统划分为：活动大陆边缘海相火山岩-盆地流体成矿系统,活动大陆边缘火山岛弧-岩浆活动成矿系统和被动大陆边缘沉积盆地-热水活动成矿系统三类。同时对形成于大陆边缘的成矿区带进行划分,主要包括：阿勒泰南缘晚古生代活动大陆边缘块状硫化物成矿带;阿尔泰南缘-东准噶尔活动大陆边缘卡拉先格尔岛弧斑岩铜金成矿带;东天山晚古生代活动大陆边缘铜钼锌成矿区带;西准噶尔洋内弧斑岩-浅成低温热液铜金成矿区带;西天山（伊犁地块）活动大陆边缘金铜成矿区带;塔里木板块被动大陆边缘沉积型铅锌成矿带。本文认为大陆增生与成矿作用的关系是矿床学和成矿系统研究的重要内容,成矿区带是成矿系统发生成矿作用的响应,而成矿系统是成矿区带形成的本质。     

陕甘宁盆地遥感地质特征

通过对1∶25万TM卫星1、4、7波段假彩色合成影像图及其东西、南北、北东及北西方向上的线性增强图,1∶3.5万和1∶5万的航空照片的解译,结合野外实地考察,得到如下结果:a.陕甘宁盆地线性断裂构造发育,可划分出东西、南北、北西、北北西、北东、北北东等6组断裂。它们在空间上呈现出近等间距性、网络格局、断续成带的特点;在活动性上具有断距小、隐伏性、强度低的特点。它们明显地控制着现代地形、地貌及水系的发育,表明陕甘宁盆地内部新构造活动较为明显。b.盆地南北遥感影像有着明显的差异,反映两者地质构造的差异性,特别是盆地南部地区存在一个基本围限了盆地南部黄土高原地区的巨大的环形影像,其边缘影像十分清晰,中间区域穿插了略呈格状的北西-北北西,北东-北北东、东西及南北向的断裂。该环形影像是盆地中南部控边构造的多期活动、复合、叠加、联合而成的综合影像,并不反映盆地南部存在整体大规模的顺时针或逆时针的环型块体转动。     

旅游资源密度的概念及其应用——以从化市旅游资源为例

传统的旅游资源分布图难以实现对大量数据的全面反映和深度挖掘.借鉴物理学中能量辐射的原理,指出旅游资源单体也将其影响力以能量的形式向周围辐射,并将旅游资源的密度看作是旅游资源辐射能大小的分布.由此提出旅游资源密度的概念.根据旅游资源的特殊性,改进人口密度的核心估计模型,提出旅游资源辐射能的计算模型.运用GIS技术,以从化...