Reversed impacts of the Arctic oscillation on the precipitation over the South China Sea and its surrounding areas in October and November     

Dong  Tianyun  Dong  Wenjie  Feng  Taichen  Zhu  Xian 《Climate Dynamics》2021,56(1-2):65-85

Climate Dynamics - The reversed impacts of the Arctic oscillation (AO) on precipitation over the South China Sea and its surrounding areas (SCSA) in October and November during 1979–2014 are...  相似文献   

Mechanisms and climatic-ecological effects of the Great Oxidation Event in the early Proterozoic     

Luo  Genming  Zhu  Xiangkun  Wang  Shuijiong  Zhang  Shihong  Jiao  Chaoqun 《中国科学:地球科学(英文版)》2022,65(9):1646-1672

Science China Earth Sciences - This paper briefly introduces the conception and research history of the Great Oxidation Event (GOE) in the early Paleoproterozoic and summarizes the primary...  相似文献   

The first extra-large helium-rich gas field identified in a tight sandstone of the Dongsheng Gas Field,Ordos Basin,China     

Peng  Weilong  Liu  Quanyou  Zhang  Ying  Jia  Huichong  Zhu  Dongya  Meng  Qingqiang  Wu  Xiaoqi  Deng  Shang  Ma  Yongsheng 《中国科学:地球科学(英文版)》2022,65(5):874-881

Science China Earth Sciences - Helium gas is a scarce but important strategic resource, which is usually associated with natural gas. Presently, only one extra-large helium-rich gas field has been...  相似文献   

Tectonic evolution and geodynamics of the Neo-Tethys Ocean     

Rixiang ZHU  Pan ZHAO  Liang ZHAO 《中国科学:地球科学(英文版)》2022,65(1):1-24

The Neo-Tethys Ocean was an eastward-gaping triangular oceanic embayment between Laurasia to the north and Gondwana to the south.The Neo-Tethys Ocean was initiated from the Early Permian with mircoblocks rifted from the northern margin of Gondwana.As the microblocks drifted northwards,the Neo-Tethys Ocean was expanded.Most of these microblocks collided with the Eurasia continent in the Late Triassic,leading to the final closure of the Paleo-Tethys Ocean,followed by oceanic subduction of the Neo-Tethys oceanic slab beneath the newly formed southern margin of the Eurasia continent.As the splitting of Gondwana continued,African-Arabian,Indian and Australian continents were separated from Gondwana and moved northwards at different rates.Collision of these blocks with the Eurasia continent occurred at different time during the Cenozoic,resulting in the closure of the Neo-Tethys Ocean and building of the most significant Alps-Zagros-Himalaya orogenic belt on Earth.The tectonic evolution of the Neo-Tethys Ocean shows different characteristics from west to east:Multi-oceanic basins expansion,bidirectional subduction and microblocks collision dominate in the Mediterranean region;northward oceanic subduction and diachronous continental collision along the Zagros suture occur in the Middle East;the Tibet and Southeast Asia are characterized by multi-block riftings from Gondwana and multi-stage collisions with the Eurasia continent.The negative buoyancy of subducting oceanic slabs can be considered as the main engine for northward drifting of Gondwana-derived blocks and subduction of the Neo-Tethys Ocean.Meanwhile,mantle convection and counterclockwise rotation of Gondwana-derived blocks and the Gondwana continent around an Euler pole in West Africa in non-free boundary conditions also controlled the evolution of the Neo-Tethys Ocean.  相似文献   

Does exploring the characteristics of emergency supplies really matter for disaster response operations?     

Zhu  Xiaoxin  Regan  David  Sun  Baiqing 《Natural Hazards》2022,110(1):175-189

Natural Hazards - This article aims to provide a quantitative study of immediate food supplies based on a three-stage analysis. Firstly, a numerical autoregressive integrative moving average...  相似文献   

Dynamic selection of emergency plans of geological disaster based on case-based reasoning and prospect theory     

Yao  Xin  Guo  Hai-xiang  Zhu  Jian  Shi  Yong 《Natural Hazards》2022,110(3):2249-2275

Natural Hazards - The Three Gorges reservoir area in the Yangtze River economic belt has frequent geological disasters. To assist decision-makers make effective emergency decisions based on their...  相似文献   

The Research on Stability of Surrounding Rock in Gob-Side Entry Driving in Deep and Thick Seam     

Jianjun  Shi  Jicheng  Feng  Rui  Peng  Quanjie  Zhu 《Geotechnical and Geological Engineering》2022,40(6):3357-3364

Geotechnical and Geological Engineering - The gob-side entry driving is driving in low pressure area, which bears less support pressure and is easy to maintain, so it is widely used. Taking the...  相似文献   

Design of optimal sand fences around a desert solar park—a case study from Phase IV of the Mohammed bin Rashid Al Maktoum Solar Park     

Yao  Zhengyi  Xiao  Jianhua  Xie  Xiaosong  Zhu  Haijun  Qu  Jianjun 《Natural Hazards》2022,113(1):673-697

Natural Hazards - Solar energy parks in desert areas must resist the encroachment of moving sand and burial by migrating dunes. It is therefore important to design economical, effective sand fences...  相似文献   

东秦岭商丹地区富铷花岗伟晶岩脉矿化特征及其地质意义     

朱伟鹏  宋公社  许锋  杨文博  吴鹏 《地质科技情报》2022,41(3):54-67

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南海北部琼东南盆地第四系陆架边缘轨迹迁移及深水沉积模式     

马畅  葛家旺  赵晓明  廖晋  姚哲  朱继田  方小宇  向柱 《地学前缘》2022,29(4):55-72

陆架边缘迁移轨迹综合受控于构造、物源、海平面和气候等多种因素,其迁移演化与深水沉积体系发育关系密切。陆架边缘迁移规律及沉积物输送体制与深水砂体预测是当前国际地学领域的热点议题。本文通过基于琼东南盆地新采集的高精度地震资料,定量表征了第四系陆架边缘轨迹,识别了低角度缓慢上升型、中等角度上升型和高角度急剧上升型等3类陆架边缘轨迹类型。2.4 Ma以来,陆架边缘轨迹时空演化可分为3个阶段且具有侧向差异性:2.4~1.9 Ma以低角度缓慢上升型为主,1.9~0.8 Ma西北部以低角度缓慢上升型为主,东北部则以中等角度上升型为主,0.8 Ma至今西北部以中等角度上升型为主,东北部以高角度急剧上升型为主。琼东南盆地第四系陆架边缘迁移轨迹研究表明:当陆架边缘轨迹角0°<α<4°时,陆坡区峡谷规模较小且下切浅,深海平原区发育多期大型海底扇沉积,块体搬运沉积(MTDs)较少;当4°<α<35°时,陆坡区峡谷规模有所增加,深海平原区海底扇沉积与块体搬运沉积均有出现;当35°<α<90°时,陆坡区峡谷发育较少但下切深,深水平原区沉积以大型块体搬运沉积为主,海底扇几乎不发育。琼东南盆地更新世以来气温不断下降,以及东亚冬季风的显著增强,物源供给增强加之海平面的下降进而导致了西北部陆架边缘表现为进积特征;研究区东北部的断裂活动频繁以及物源供给弱,导致了研究区东北部陆坡推进距离远远小于研究区西北部且发育多期次块体搬运沉积物。以上认识对南海北部陆架边缘体系及深水扇预测具有一定的理论意义。  相似文献