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Karst相关的网络例句

查询词典 Karst

与 Karst 相关的网络例句 [注:此内容来源于网络,仅供参考]

The chief controlling factors to available reservoir are paleo-karst morphology in Llandeilo to Early Caradoc and multi-stage faulting and karstificatio. Its evolution of reservoir chiefly suffered the reconstruction of diagenesis such as epidiagenetic karstifiration uncovered for over 10 Ma in Llandeilo to Early Caradoc and 3-stage burial karstification since Late Ordovician to Devonian, Permian to Triassic and Tertiary.

有效储集层主控因素是兰代洛世-卡拉道克世早期的岩溶古地貌及多期断裂岩溶作用,其储集空间演化主要经历了兰代洛世-卡拉道克世早期长达10×10^6a以上的暴露淡水岩溶及3期(晚奥陶世-泥盆纪、二叠纪-三叠纪、古近-新近纪以来)埋藏岩溶等建设性成岩作用的改造。

Summarizing and analysing the stability of stratigraphy and the basic characteristics of geological hazard at the Three Gorges Reservoir,the authors put forward the dangerous slope mainly includes bedding slope,hard and soft rock alternation gentle slope,loose accumulative slop,karst breccia slop and layer cataclastic rock slop.The loose accumulative slopes from Fengjie to Badong are most dangerous and need to control.

在总结分析三峡水库区岩层稳定性及地质灾害基本特征的基础上,根据岩性和结构特征,提出三峡水库区存在较为严重失稳隐患的边坡主要有顺层边坡、平缓软硬岩层互层边坡、松散堆积体边坡、岩溶角砾岩边坡和层状碎裂岩边坡等5种类型,其中分布于奉节至巴东段的松散堆积体边坡危险性最大,是需工程防护的重中之重。

Carbonate fractured/caverned karst reservoirs are a kind of composite ones that are superimposed by many fracture/cavern units within the control of cyclical tectonics and karstification so this kind of reservoirs are more difficult exploration and development than other kind of ones.

碳酸盐岩岩溶缝洞型油气藏是受构造—岩溶旋回作用控制、由多个缝洞单元在空间上叠合形成的复合油气藏,勘探开发难度比较大。塔河油田是我国第一个以奥陶系碳酸盐岩岩溶缝洞型油气藏为主的古生界海相大油气田,勘探开发有其特殊性和复杂性。

Keywords Carbonate reservoir;Karst reservoir;Fractured and caverned reservoir;Oil and gas exploration;Exploration technology;Development technology;Tahe Field;Tarim Basin

碳酸盐岩油气藏;岩溶油气藏;缝洞型油气藏;油气藏勘探;勘探技术;开发技术;塔河油田;塔里木盆地

Rainfalls can " deposit " the co2 in air , making it to take part in the process of karst , to dissolve and corrade carbonate rock . co2 concentration in soil become lower after heavy rainfall and become higher after general rainfall .( 8 ) the value of chemical characteristic of soil water in the high elevation area is lower than that in the low elevation area

降雨可以对coz产生影响,&沉淀&大气中的co :,使其参与到岩溶作用中,溶蚀碳酸盐岩;降雨对土壤空气中coz的影响与雨强、雨量有关,降雨量、雨强较大时,土壤空气中的c02产生受到抑制,降雨量和雨强较小时,土壤空气中的coz浓度升高。

Those three classes of ecosystem are:(1) peak cluster-narrow valley system;(2) karst hill, stone forest, peak clusler-wide valley, shallow depression system;(3) peak cluster-deep depression, dolina system.

因此,西南喀斯特山区生态系统的划分应将人类活动干扰程度和喀斯特地貌所造成的差异结合起来进行。

Well-developed Karst landform cover the whole area such as awl peak, steep mountains, underground water, cascades, caverns, doline, depression land, and valleys.

区内喀斯特地貌极为发育,锥峰、峻岭、暗河、瀑布、溶洞、漏斗、洼地、峡谷遍布景区。

The leaching and release of Ca~(2+) and HCO_3, the key elements for karstification, is characterized by a first high concentration but fast decreasing phase followed by a phase steady to equilibrium, indicating removal of readily mobile Ca and bicarbonate is involved in epigenic limestone dissolution as evaluated by karst water chemistry.

结果表明,岩溶作用使土壤中易移动性组分淋溶,Ca~(2+)、HCO_3~-的淋出动态表现为开始的快速下降和随之的平衡两个淋出阶段,淋出量与土壤中水溶性Ca、可氧化有机质的含量有关。土壤对HCO_3~-的淋出与排释有促进作用。

Changes, the park's karst landscape is extremely complex with many geomorphic features of

于剧烈的地壳运动,丰芽格邦国家公园的喀斯特地貌异常复杂,具有许多重要的地貌特征。

Subject to massive tectonic changes, the park's karst landscape is extremely complex with many geomorphic features of considerable significance.

由 于剧烈的地壳运动,丰芽格邦国家公园的喀斯特地貌异常复杂,具有许多重要的地貌特征。

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