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71.
通过对兰坪盆地野外露头及相关室内研究,分析了区内古近纪的沉积环境、层序特征、沉积相展布及其演化特征。认为古近纪主要发育冲积扇、河流、三角洲和湖泊环境。沉积建造为一个完整的盆地演化旋回:低位期,印度板块向欧亚板块的俯冲挤压造成兰坪走滑拉分盆地的形成,沉积了一套局限的湖盆相红色含膏盐细碎屑岩建造;湖扩期,挤压应力场转变为拉张应力场,湖盆扩大,大面积沉积了一套滨浅湖相紫红、砖红色砂泥岩互层沉积;湖缩期,受晚始新世喜马拉雅运动一幕的影响,应力场再次转变为强烈挤压,东西两侧造山带共同向盆地内推覆扩展,致使盆地范围明显缩小,仅在推覆体前缘形成一系列快速充填的小型山前陆相前陆盆地。层序古地理编图显示,蒸发岩发育于低位体系域,与低位期的沉积充填特点和气候有关,极具有找钾盐矿的前景。 相似文献
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Regional Distribution and Prospects of Potash in China 总被引:4,自引:0,他引:4
ZHENG Mianping an ZHENG Mianping YUAN Heran LIU Xifang CHEN Wenxi LI Jinsuo 《《地质学报》英文版》2011,85(1):17-50
China was formed by amalgamation of several small continental blocks (cratons), micro, blocks and orogenic belts in different paleoclimatic settings. It may be correlated with other continental blocks but has its own specific characteristics; therefore the tectonic environments of China’s marine and continental saline basins and salt, and potash, forming environment have some specific characteristics: multiple phases of salt formation, difference in salt, forming ages, migration and concentration of salt, forming processes and diversity of component materials, as well as small sizes of marine saline basins and great changes of saline basins in the late stage and occurrence of abundant liquid mineral resources. The nature of the tectonic basement exerted a key controlling effect on the formation of potash basins. The stable tectonic region was favorable for potash concentration in a quasi, stable region, and quasi, and the quasi-stable region was favorable for salt concentration and potash formation in a local stable tectonic region. Most China’s major ancient saline basins occur in “quasi, cratons (continental block)”; especially all the marine saline basins occur in continental blocks with the Precambrian basement. These regions are the key ones for potash search. Most relatively large, scale soluble salt deposits are developed in relatively stable continental nuclei. According to the characteristics of the tectonic domains where China’s salt, forming basins are located, the North China, Yangtze and Tarim, Qaidam salt minerogenetic domains and the northern Qiangtang, western Yunnan salt minerogenetic belt may be distinguished. Their salt and potash prospects will be discussed separately. 相似文献
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Lake St Lucia in South Africa is part of a UNESCO World Heritage site and a Ramsar wetland of international importance. Like many coastal wetlands worldwide, anthropogenic activities including catchment land-use changes, water diversions/abstractions, and manipulation of the mouth state have significantly affected its functioning over the past century. Questions concerning its sustainability have motivated a re-evaluation of management decisions made in the past and of options for the future. A model for the water and salt budgets has therefore been used to investigate “what if” scenarios in terms of past anthropogenic interventions. In particular, simulations allow us to evaluate the effects of diverting the Mfolozi river from St Lucia on the functioning of the system and on the occurrence of various water level/salinity states that drive the biological functioning of the ecosystem. In the past, when the St Lucia estuary and the Mfolozi river had a combined inlet, the mouth was predominantly open. The lake had relatively stable water levels but variable salinities that increased during dry conditions due to evaporative losses and saltwater inflows from the sea. If the mouth closed, the Mfolozi flow was diverted into the lake which reduced salinities and maintained or increased water levels. Simulations indicate that without a link to the Mfolozi the lake system would naturally have a mainly closed inlet with lower average salinities but more variable water levels. During dry conditions water levels would reduce and result in desiccation of large areas of the lake as has recently occurred. We conclude that the artificial separation of the St Lucia and Mfolozi inlets underpins the most significant impacts on the water & salt budget of the lake and that its reversal is key to the sustainability of the system. 相似文献
77.
天津近海潮汐特征分析 总被引:1,自引:0,他引:1
对塘沽海洋环境监测站从1950年-2008年,59年的潮汐资料进行调和分析,分析了其分潮调和常数的变化曲线,并利用FFT谱分析方法对其调和常数的变化周期和原因进行了分析;之后应用FFT谱分析方法对去除天文潮后的余水位进行分解,分析了近50多年来年平均余水位的多层次周期分布,进而利用最小二乘法进行线性分析,分析了天津近海... 相似文献
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