大别造山带南坡晚白垩世玄武岩源区地幔特征   总被引：9，自引：1，他引：9  

匡少平  张本仁  凌文黎  韩吟文 《地质科学》2001,36(2):203-211

大别造山带南坡中生代断陷盆地中出露大量晚白垩世碱性玄武岩类。因岩浆受结晶分异和陆壳混染影响微弱,其成分基本可代表本区原生玄武岩浆。在微量元素原始地幔标准化蛛网图上,本区玄武岩具有地壳富集组分Pb、K、Rb、Ba等的正异常和Nb、P、Hf等高场强元素的负异常。同位素和微量元素特征显示,玄武岩浆来自亏损地幔(DM)和富集地幔(EM+EM)混合源区。玄武岩源区地幔中Pb的富集和Nb、P、Hf等的亏损基本可由中国东部亏损地幔与榴辉岩的混合获得,由此揭示富集地幔端元组成特征可能与晚白垩世前造山带根部榴辉岩拆沉并参与地幔再循环有关。  相似文献   

准噶尔盆地西缘二叠-三叠系扇控成岩储集相成因机理   总被引：24，自引：5，他引：19  

邹才能  侯连华  匡立春  况军 《地质科学》2007,42(3):587-601

对准噶尔盆地西缘前陆冲断背景下形成的扇控沉积储层特征的研究,发现沉积、构造、流体和热演化4种机制是主要的成岩成孔作用,各自的成因机理不同,据此提出了4种成岩储集相成因机制和相应的发育模式。指出二叠-三叠系储层孔隙空间主要以溶孔为主,发育粘土收缩孔缝、粒内缝、颗粒溶蚀、沸石溶蚀、构造缝及气孔等多种成岩储集相。不同成岩成孔机制相互配合是形成该区有利成岩储集相的条件,预测断裂发育区油气勘探有利埋深度可达7000m,非断裂发育区油气勘探有利埋藏深度可达4500m,改变了原来对该地区有效储集层埋藏下限深度为3500m的观点。这对我国类似地区的有利成岩储集相预测具有理论参考价值,对油气勘探具有指导作用。  相似文献   

广东惠州燕山期以来地质构造演化:对华南构造的新启示          下载免费PDF全文

张敏  旷健  肖志才  王帅  祁士华  陈孝雄  李立峰  唐灵 《地球科学》2021,46(1):242-258

为揭示广东惠州燕山期以来的地质构造演化,以惠州石坝-黄沙洞地区为例,并综合基础地质调查、大地电磁学、岩石地球化学、年代学等方法来分析研究.大地电磁结果显示研究区深部存在连为一体厚超5 km的燕山期花岗岩体岩床,并被新生代断裂切割;丹霞组底砾岩矿物磨圆较差显示出近源沉积特征;谐和年龄及年龄谱图揭示底砾岩年龄约160 Ma...  相似文献   

冀中坳陷束鹿凹陷古近系沙河街组三段泥灰岩成因探讨   总被引：8，自引：3，他引：5  

梁宏斌  旷红伟  刘俊奇  郭永军  苏静 《古地理学报》2007,9(2):167-174

冀中坳陷束鹿凹陷中部古近系沙河街组三段下部（简称沙三下）泥灰岩属一类特殊的岩石类型组合,既非典型的碳酸盐岩,又非经典的碎屑岩。在进行了详细的岩心、薄片观察和各种分析化验资料的综合分析基础上,认识到研究区岩石为混积岩类,将混积岩（广义的）、混合沉积的概念和体系引入沉积物类型和岩相的划分中,为泥灰岩的科学定名提供了依据。据此对混积岩的类型进行了细致的划分,共划分出3大类型：结构混合、互层混合和夹层混合。每一类可以再细分为多种,其中结构混合包括①陆源组分为主的混积岩,②以内源组分为主的混积岩。互层混合成因的混积岩是最重要的岩石类型,本区所谓的纹层状泥晶灰岩大部分属于这一沉积类型,主要由灰质泥岩或泥灰岩与泥晶灰岩组成明暗相间的条带,有时含丰富的有机质。互层出现的形式是多种多样的,依据其岩石中原地组分和异地组分的含量不同,可进一步划分为4种类型。夹层混合沉积,表现为巨厚的碳酸盐岩质砾岩层夹前两类混积岩。构造、气候及物源等是控制混积岩形成的主要因素。  相似文献   

Timing and mechanism of reservoir forming in the Upper Triassic Halahatang Formation,Yuqi block,Tarim Basin,northwestern China     

Lixiong Kuang  Hao Zheng  Mingyan Wang  Taizhu Huang  Chensheng Liu 《Marine and Petroleum Geology》2010

The Yuqi block is an important area for oil and gas exploration in the northern Akekule uplift, Tarim Basin, northwestern China. The Upper Triassic Halahatang Formation (T₃h) within the Yuqi block can be subdivided into a lowstand system tract (LST), a transgressive system tract (TST), and a highstand system tract (HST), based on a study of initial and maximum flood surfaces. Oil in the lowstand system tract of the Halahatang Formation is characterized by medium to lightweight (0.8075 g/cm³–0.9258 g/cm³), low sulfur content (0.41%–1.4%), and high paraffin content (9.65%–10.25%). The distribution of oil and gas is principally controlled by low-amplitude anticlines and faults. Based on studies of fluorescence thin sections and homogenization temperatures of fluid inclusions, reservoirs in the T₃h were formed in at least two stages of hydrocarbon charge and accumulation. During the first stage (Jurassic–Cretaceous) both the structural traps and hydrocarbon reservoirs were initiated; during the second stage (Cenozoic) the structural traps were finally formed and the reservoirs were structurally modified. The reservoir-forming mechanism involved external hydrocarbon sources (i.e. younger reservoirs with oil and gas sourced from old rocks), two directions (vertical and lateral) of expulsion, and multi-stage accumulation. This model provides a theoretical fundament for future oil and gas exploration in the Tarim Basin and other similar basins in northwestern China.  相似文献   

Research progress and prospects of digital restructuring of global-local interactions北大核心CSCD     

Kuang A.  Wang M.  Zhang Y. 《地理科学进展》2023,(2):380-391

Global-local interaction is an important research topic in economic geography. In recent years, the rapid development of digitalization in various countries and regions has profoundly affected the global production and trade networks. However, there is a lack of systematic theoretical discussion on digitalization and global-local interaction studies. The objective of this study is to conceptually rethink the role of digitalization in reshaping global-local interactions from a dynamic and relational perspective. To do this, the study first systematically reviewed the digital turn in economic geography and discussed the rethinking of digitalization. It is found that the understanding of digitalization is gradually moving beyond the limits of isolated, static, and passive technocentric approaches and towards a more dynamic, relational, and open perspective. Second, the study combined the "digital turn" with the "relational turn" in relational economic geography, which constructs theoretical bridges between digitalization and global-local studies. Third, this study provided a basic understanding for sorting out the evolution of the research frameworks, that is, from the global value chain (GVC) to the global production network (GPN) and then to the digital ecosystem (DE). We argued that digitalization has been deeply involved in shaping the global economic landscape, restructuring global-local production relations, and reconstructing regional development. Based on this recognition, we discussed the primary performance of digitalization on the restructuring of global-local interaction from three aspects: enterprise relationship, spatial effect and interaction mechanism. Finally, grounded in the practice of China's urban and regional digital economy development, the possible theoretical innovations and prospects for future research on digitalization and global-local interaction in the Chinese context were proposed. The study pointed out that we can integrate the regional practices of China's digital development with more in-depth research from the perspectives of the platform ecosystems, spatial effects, location analysis, local development models, and so on in future research. © 2023, Editorial office of PROGRESS IN GEOGRAPHY. All rights reserved.  相似文献   

1986—2021年国家自然科学基金资助大气科学研究35年     

匡钰  王卓妮 《气象科学进展》2022,(1)

中国基础科学全面发展的一个重要标志,是1986年国家自然科学基金委员会的建立。从该年开始,基金委地学部开始资助大气科学基础研究项目。截至2021年,35年来,基金委以研究项目的遴选、资助和评估等过程为推动,不仅促成了我国大气科学研究的持续进步,更形成了一支核心研究机构和队伍。自然科学基金大气科学类项目立项呈现持续增加态势立项数量的增加出现两个快速增加的台阶:一是2000年开始。  相似文献