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Rio Grande an International Boundary River Is Drying up and in Need of Restoration
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作者 Kenneth R. Olson James M. Lang 《Open Journal of Soil Science》 2021年第12期587-610,共24页
The headwater source of the Rio Grande is in the Colorado San Juan Mountains as it flows southeast and south. The river crosses deserts and steppes, watering rich irrigated agricultural regions as it drains into the G... The headwater source of the Rio Grande is in the Colorado San Juan Mountains as it flows southeast and south. The river crosses deserts and steppes, watering rich irrigated agricultural regions as it drains into the Gulf of Mexico near Brownsville, Texas. The river flow pattern is disrupted by hundreds of dams and irrigation diversions, which has left sections of the Rio Grande River dry. The lower Rio Grande Valley including the Rio Grande Delta is heavily irrigated and has become an important agricultural region. Since the mid-1990s, the flow has been reduced to 20% because of many large diversions, dams and consumption of water by cities and irrigated farmland. Even with a series of 2001 and 2002, Mexico-United States agreements administered by the International Boundary and Water Commission (IBWC) the Rio Grande River had continued to failed to reach the Gulf of Mexico. Mexico and United States share the river. Historically, the Rio Grande has provided limited navigation and border security. There is a need to restore navigation and shipping by creating a lock and dam system from El Paso, Texas and Matamoros, Mexico to the Gulf of Mexico, In addition there is also a need to restore border security for the Lower Rio Grande, an international border river. If the Rio Grande is ever going to recover, it will require a lock and dam system and an increased river flow. The increased flow needs to be achieved by adding additional water from feeder lakes, a water pipeline, and a balanced approach to water management must include efficiency measures and aggressive conservation in urban areas and on irrigated agricultural lands. 展开更多
关键词 Big Bend National Park Mexico Border Brownsville and Matamoros International Bridge Port Brownsville rift cross section Thornforest RESTORATION
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琼东南盆地北部地区对倾叠覆型变换带形成演化及成因分析 被引量:3
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作者 赵海涛 郭进京 刘重庆 《油气地质与采收率》 CAS CSCD 北大核心 2020年第6期11-19,共9页
为进一步认识裂陷盆地对倾叠覆型变换带形成和演化过程,根据地震反射资料和平衡剖面技术对琼东南盆地北部地区松西-松东变换带进行构造解析。结果表明,松西-松东变换带属于5号断层和6号断层之间的对倾叠覆型变换带,其发育过程可分为初... 为进一步认识裂陷盆地对倾叠覆型变换带形成和演化过程,根据地震反射资料和平衡剖面技术对琼东南盆地北部地区松西-松东变换带进行构造解析。结果表明,松西-松东变换带属于5号断层和6号断层之间的对倾叠覆型变换带,其发育过程可分为初始发育(始新世)、定型发育(崖城组沉积时期)、稳定发育(陵水组沉积时期)和消亡发育(三亚组沉积时期)等4个演化阶段。根据现有变换带成因理论及平衡剖面分析结果,松西-松东变换带主要是由于5号断层和6号断层分段生长作用造成的,其形成演化过程可以采用应力降低带理论进行解释。在裂陷阶段松西-松东变换带始终处于构造高部位,可同时捕集两侧凹陷生成的油气,且受应力降低带影响形成的大量次级断层及盆地抬升期间的风化剥蚀能有效改善储集性能,具有极为有利的油气成藏条件。 展开更多
关键词 变换带 裂陷盆地 平衡剖面 断层分段生长 应力降低带 琼东南盆地
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