THE LIFE-CYCLE OF MINERAL CONSUMPTION IN REGIONAL DEVELOPMENT AND ITS IMPLICATION     

Zhang Lei Institute of Geography  CAS  Beijing People''s Republic of China 《地理学报(英文版)》1997,(2)

Ｉ.ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｒｏｕｇｈｏｕｔｈｉｓｔｏｒｙｍｉｎｅｒａｌｓｈａｖｅｂｅｅｎａｄｅｔｅｒｍｉｎａｎｔｆａｃｔｏｒｉｎｔｈｅｅｖｏｌｕｔｉｏｎｏｆｓｏｃｉｅｔｉｅｓａｎｄｃｉｖｉｌｉｚａｔｉｏｎ.ＴｈｅｖｅｒｙｏｂｖｉｏｕｓｉｍｐａｃｔｏｆｍｉｎｅｒａｌｓｏｎＭａｎ’ｓｅｖｏｌｕｔｉｏｎｃａｎｂｅｔｒａｃｅｄｉｎｔｅｒｍｓｏｆＭａｎ’ｓａｃｑｕａｉｎｔａｎｃｅｗｉｔｈｍｉｎｅｒａｌｓ—ｔｈｅＰｒｅｓｔｏｎｅＡｇｅ,ｔｈｅＳｔｏｎｅＡｇｅ,ｔｈｅＢｒｏｎｚｅＡｇｅ,ｔｈｅＩｒｏｎＡｇｅ,…  相似文献   

鲁西地壳隆升的伸展构造模式   总被引：23，自引：2，他引：23  

燕守勋 《地质学报》1996,70(1):1-11

伸展链锁断层系，形成了鲁西的主导造格局，即“块断”构造。它是由中、生代两次伸展运动形成的。伸展运动幔源岩浆活动有着密切的成生联系。伸展运动的结果，形成了以泰山－鲁山－沂山为核心的鲁中块隆，它至今耸立于周围以平原地貌为标志的地堑系之间，隆起的高点，就是当今的泰山。  相似文献   

Screening Effect of the Diffusive Boundary Layer in Sediments of Lake Aha in the Suburbs of Guiyang City,Guizhou Province   总被引：6，自引：0，他引：6  

万国江  万曦等 《中国地球化学学报》1997,16(4):347-352

The redox cycle of iron and manganese is a major geochemica process at the boundary layers of lake sediments.Lake Aha,which lies in the suburbs of Guiyang City,Guizhou Province,China,is a medium-sized artificial reservoir with seasonally anoxic hypolimnion,Long-term sedimentary accumulation of iron and manganese resulted in their enrichment in the upper sediments,In the anoxic season,Fe^2 and Mn^2 ,formed by diological oxidation,would diffuse up to overlying waters from sediments.However,the concentration of oxidation,would diffuse up to overlying waters from sediments,However,the concentration of Fe^2 increased later and decreased earlier than that of Mn^2 .Generally,sulfate reduction occurred at 6 cm below the sediment-water interface.Whereas,in the anoxic season.the reduction reached upper sediments,inhibiting the release of Fe^2 ,The Fe concentration of anoxic water is quickly decreased from high to low as a result of reduction of the suplhur system.  相似文献   

江西广丰地区中奥陶统层序地层分析     

李晓勇 《江西地质》1997,11(2):20-24

本文通过对广丰县周家坞中奥陶统露头剖面层序、体系域、副层序的研究，识别出了三个不同性质的Ⅱ型层序界面和二个三级层序，确认这三个层序界面为符合实际又易于野外识别的自然界面，并对ＳＱ２中反映最大海泛期的高分辨异旋回驱动机制事件，提出可能受米兰柯维奇频率的春分点和秋分点间约２万年间隔的控制。  相似文献   

An urban hydrological model with high spatial resolution rainfall from a meteorological model     

J. Thielen  J. -D. Creutin 《Journal of Hydrology》1997,200(1-4):58-83

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陕西关中晚更新世黄土—古土壤序列特征及其记录的古环境变迁   总被引：7，自引：1，他引：7  

雷祥义  岳乐平 《地质论评》1997,43(5):555-560

陕西关中盆地的泾阳南塬和西安东郊席王晚更新世黄土剖面底部的Ｓ１古生境是由４层古土壤及与其相间的两层古土壤构成。这是目前发现的黄土高原晚更新世黄土，古土壤序列保存较好的剖面。两剖面的地层结构，磁化率曲线和地球化学组分反映出了１２个温湿，冷干气候变化阶段可以归纳为６个气候变化旋回。  相似文献   

Sequence Stratigraphy of the Permian--Triassia Boundary Section of Changxing, Zhejiang, Southern China   总被引：1，自引：0，他引：1  

Zhang Kexin  Tong Jinnan  Yin Hongfu  Wu Shunbao China University of Geosciences  Wuhan  Hubei 《《地质学报》英文版》1997,71(1):90-103

Three third-order sequences and about one hundred high-frequency cycles or Milankovitchcycles within the Late Permian Changxingian to Early Triassic Griesbachian are identified in theMeishan Section of Changxing, Zhejiang Province, southern China, the candidate stratotype sec-tion of the global Permo-Triassic boundary, based on a detailed study of the biological,ecological and high-resolution allochthonous cyclic events, microfacies and depositional systems.Furthermore, the stacking pattern of the depositional systems across various Changxingian andGriesbachian sedimentary facies of the Lower Yangtze and the sequence stratigraphic frameworkare outlined with the Meishan section as the principal section. In this paper the habitat types offossil biota are applied to semiquantitative palaeobathymetry and the study of relative sea levelchanges.  相似文献   

Quantitative Tectonic Markers of Large Coastal Earthquakes in Fujian, Guangdong, Taiwan and Hainan——with a Discussion of Qualitative Indicators     

Bi Fuzhi Yuan Youshen Institute of Crustal Dynamics  State Seismological Bureau  Beijing 《《地质学报》英文版》1997,71(4):395-406

This paper expounds the quantitative tectonic indicators and some qualitative indicators of large earthquakes in the coast areas of Fujian, Guangdong, Taiwan and Hainan. The main quantitative indicators include uplift amplitude of the Moho, Quaternary and Late Holocene coasts. The paper also gives a brief account of the research method on quantitative indicators of surface uplifted zones. Taiwan is a famous neotectonic zone and an area of large earthquakes in the world. There is only one large-earthquake area in each of Fujian, Guangdong and Hainan Provinces. Along the coast large earthquake areas there are certainly many remains of crustal activity. Among these remains, coast activity, taking the sea level as the accurate marker horizon, can determine not only the amplitude of coastal elevation and subsidence in a certain period, but also the cycle and rate of positive or negative movements.  相似文献   

100Ma——塔里木盆地演化的重要周期   总被引：6，自引：0，他引：6  

李京昌  金之钧  刘国臣  张一伟 《地学前缘》1997,(Z2)

运用沉积盆地波动分析方法对塔里木盆地典型井的周期分析表明，塔里木盆地在其地质历史时期１００Ｍａ的周期是很明显的，自寒武纪以来共经历了４个完整的周期，每一完整周期都由正相位和负相位两个半周期所组成，而第三纪为第Ⅴ个周期的正相位阶段。该周期控制了盆地内的沉积与剥蚀的过程及成藏旋回，并至少控制了古生代的反转构造。对沉积与剥蚀过程的控制作用表现在周期波正相位和负相位分别对应于沉积期和剥蚀期；对含油气系统的控制作用表现在：第Ⅰ个周期波构成以早古生代地层为主体的含油气系统，第Ⅱ个周期波至第Ⅳ个周期波构成以晚古生代至中生代地层为主体的含油气系统，第Ⅴ个周期的正相位阶段构成以新生代地层为主体的含油气系统；对反转构造的控制作用表现在：正相位Ⅰ（寒武纪—早奥陶世）和正相位Ⅱ（晚泥盆世晚期—晚石炭世早期）为伸展构造体制，负相位Ⅰ（中奥陶世—晚泥盆世早期）与负相位Ⅱ（晚石炭世晚期—早二叠世早期）为挤压构造体制。塔里木盆地演化具有１００Ｍａ周期的原因与古天山洋、古昆仑洋及特提斯洋的Ｂ型俯冲触发的地幔羽的上升流及地块的拼贴导致的地幔羽的休眠状态息息相关，从而周期性地控制了塔里木盆地内的沉积与剥蚀过程、成藏旋回及反转构造。  相似文献   

ANALYSIS OF THE RELATIONSHIP BETWEEN THE CHINA ANOMALOUS CLIMATE VARIATION AND ENSO CYCLE ON THE QUASI-FOUR-YEAR SCALE     

朱艳峰  陈隆勋  宇如聪 《热带气象学报(英文版)》2004,10(1):1-13

1 INTRODUCTION Much work has been done addressing the relationship between anomalous climate changes and ENSO in China and the results vary much. For instance, Li et al. (1987) [1] think that the Mei-yu (sustained rain) starts later, lasts shorter and pre…  相似文献