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湖泊和湖泊沉积呈现出两个基本的争论点:(1)现代湖泊非常复杂,但湖泊的岩石记录相对简单,对其大量的观察反映了共同和广泛出现的三种不同的相组合这里把这些相组合称为河流—湖泊相组合、波动深湖相组合和蒸发岩相组合;(2)对现代和古代湖泊的大多数解释都将它们的自然特征归因于气候条件,但现代湖泊参数(湖泊大小、深度和盐度)和古代湖泊地层特征(厚度、范围、岩性)都与测量或推测的气候湿度不一致。我们提出是潜在的可容空间(大多数是构造的)与沉积物+水充填(大多数为气候的函数)速率的相对平衡控制了湖泊的发生、分布和特征。根据这些速率间的平衡,可将湖盆称为过充填的、平衡充填的或欠充填的。我们的结论是,气候条件和构造活动对中等规模(1米至几百米)和大规模(几百米至几千米)湖泊沉积都产生了等同的影响。
Lake and lake sedimentation present two basic contentions: (1) Modern lakes are complex, but lakes have relatively simple rock recordings and their large number of observations reflect three common and widely occurring combinations. These are The combination is called a combination of a river and a lake, a combination of undulating deep-lacustrine facies and an evaporite. (2) Most interpretations of modern and ancient lakes attribute their natural characteristics to climatic conditions, but modern lake parameters Lake size, depth and salinity) and ancient lake stratigraphy (thickness, extent, lithology) are all inconsistent with the measured or estimated climate humidity. We propose that the relative balance of the potential accommodation space (mostly constructed) with the rate of sediment + water filling, most of which is a function of climate, controls lake occurrence, distribution and characteristics. Depending on the balance between these rates, the lake can be referred to as over-filled, balanced-filled or under-filled. We conclude that climatic conditions and tectonic activities have the same effect on medium-sized (1 to hundreds of meters) and large-scale (hundreds to thousands of kilometers) lake deposits.