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Many turbidite sandstone bodies, deposited during the Middle Miocene to Pliocene, are distributed and form one of major reservoirs for oil and gas in the Tertiary Niigata backarc sedimentary basin, the most productive oil basin in the Japanese Islands. We conducted detailed and systematic heavy mineral analysis for these turbidite sandstone bodies with following purposes and results.Firstly, the authors show a typical case study that the positive combination of heavy mineral analysis with sedimentological analysis...

Many turbidite sandstone bodies, deposited during the Middle Miocene to Pliocene, are distributed and form one of major reservoirs for oil and gas in the Tertiary Niigata backarc sedimentary basin, the most productive oil basin in the Japanese Islands. We conducted detailed and systematic heavy mineral analysis for these turbidite sandstone bodies with following purposes and results.Firstly, the authors show a typical case study that the positive combination of heavy mineral analysis with sedimentological analysis leads to a completely different idea on the sedimentary process. Detailed vertical and lateral heavy mineral analysis of the early Pliocene turbidite sandstone body, located at the eastern margin of the basin, disclosed that heavy mineral composition of the turbidite sandstones in the eastern half of the body are completely different from that in the western half of the body. The results of heavy mineral and sedimentological analysis convinced that two kinds of turbidite sandstones, shallow marine shelf turbidite sandstones in the eastern half and deep marine submarine fan turbidite sandstones in the western half, were juxtaposed in the area during the early Pliocene age. Secondly, the authors verify the effectiveness of heavy mineral composition as useful indicators to characterize the individual turbidite bodies which occupy the specific spaces with specific formation names or member names. Many turbidite sandstones located in the middle part of the Niigata basin has been selected for this purpose and resulted in the following conclusions. (1) The turbidite sandstones in the study area can be classified at least into six types based on the combination of the quantitatively major heavy minerals such as opaque minerals, hornblende, hypersthene, and augite. (2) The turbidite sandstones of one formation or one member are represented by one type or closely related two types. (3) The different formations or members in the study area are often composed of the different heavy mineral composition. The different provenance or the different geologic event (e.g. the beginning of volcanic activities) at the same provenance may be suggested as a cause of the difference.As a conclusion, the heavy mineral analysis is valuable not only as a conventional tool to estimate the provenance, but also as a strong measure to disclose their sedimentary process in combination with other sedimentary data, to estimate the original relationship of several sandstone bodies neighboring each other , and to predict the three-dimensional extents of surface and subsurface turbidite sandstone bodies.

沉积于中中新世到上新世的浊积砂体是第三纪Niigata弧后盆地的主要油气储层之一 ,该盆地是日本列岛最富产石油的盆地。我们对这些浊积砂体的重矿物进行了详细和系统地分析。首先 ,作者展示了将重矿物分析和沉积作用分析相结合 ,从而得出有关沉积过程的全新观点的实例。沿着位于盆地东缘的上新世早期的浊积砂岩体的垂向和横向取样分析表明 ,砂体东半部重矿物的成分和西半部重矿物的成分不同。重矿物和沉积分析结果表明 ,发育在东半部的浅海陆架浊积砂岩和发育在西半部的深海水下浊积体在上新世早期是相互叠置的。其次 ,作者检验了用重矿物成分作为指标来表征某个特定浊积体的有效性。为此目的特选重位于Ni igata盆地中部的许多浊积砂岩分析研究 ,得出以下结论。 ( 1)基于主要重矿物 ,比如蛋白石、普通角闪石、紫苏辉石和普通辉石的定量综合分析 ,至少可将研究区的浊积砂岩划分为 6种类型 ;( 2 )一个组或段的浊积砂岩包括一种类型或紧密相关的两种类型 ;( 3)研究区不同的组或段通常由不同的重矿物组成构成 ,不同的物源或相同物源下不同的地质事件 (例如火山活动开始期 )可能是这种差异的原因。重矿物分析不仅可作为有价值的常规手段估计物源方...

沉积于中中新世到上新世的浊积砂体是第三纪Niigata弧后盆地的主要油气储层之一 ,该盆地是日本列岛最富产石油的盆地。我们对这些浊积砂体的重矿物进行了详细和系统地分析。首先 ,作者展示了将重矿物分析和沉积作用分析相结合 ,从而得出有关沉积过程的全新观点的实例。沿着位于盆地东缘的上新世早期的浊积砂岩体的垂向和横向取样分析表明 ,砂体东半部重矿物的成分和西半部重矿物的成分不同。重矿物和沉积分析结果表明 ,发育在东半部的浅海陆架浊积砂岩和发育在西半部的深海水下浊积体在上新世早期是相互叠置的。其次 ,作者检验了用重矿物成分作为指标来表征某个特定浊积体的有效性。为此目的特选重位于Ni igata盆地中部的许多浊积砂岩分析研究 ,得出以下结论。 ( 1)基于主要重矿物 ,比如蛋白石、普通角闪石、紫苏辉石和普通辉石的定量综合分析 ,至少可将研究区的浊积砂岩划分为 6种类型 ;( 2 )一个组或段的浊积砂岩包括一种类型或紧密相关的两种类型 ;( 3)研究区不同的组或段通常由不同的重矿物组成构成 ,不同的物源或相同物源下不同的地质事件 (例如火山活动开始期 )可能是这种差异的原因。重矿物分析不仅可作为有价值的常规手段估计物源方向 ,而且可同其他的沉积资料结合来解析沉积过程 ,估计几个相邻

Glucksberg (1999, 2003) and his co-researchers (Glucksberg & Keysar 1990,Glucksberg & McGlone 1999) proposed the class-inclusion theory of metaphor in which comprehension is conceived as a search for an ad hoc "attributive category" and for its attributes which are exemplified by the metaphor vehicle. They conclude that metaphors embody the communicative strategy of dual reference-using prototypical category member names to identify non-lexicalized categories. A statistical analysis of the metaphor data...

Glucksberg (1999, 2003) and his co-researchers (Glucksberg & Keysar 1990,Glucksberg & McGlone 1999) proposed the class-inclusion theory of metaphor in which comprehension is conceived as a search for an ad hoc "attributive category" and for its attributes which are exemplified by the metaphor vehicle. They conclude that metaphors embody the communicative strategy of dual reference-using prototypical category member names to identify non-lexicalized categories. A statistical analysis of the metaphor data in Glucksberg and his co-researchers' papers has shown that almost all of them are hyperbolic metaphors. By examining issues such as ad hoc pragmatic scalars and scalar implicatures of hyperbolic metaphors, we incorporate those aspects of metaphors which Glucksberg et al. have not yet taken into account. The derivation of scalar implicatures of hyperbolic metaphors parallels that of hyperboles in that the exaggerated reference point highlights its neighboring target point in the scalar model as a result of the interactions and tensions between the metaphorical proposition and the ad hoc scalar model constructed with the sources from the background. We conclude that the central communicative function of hyperbolic metaphors lies in triggering scalar implicatures rather than aiming for dual reference.

Glucksberg(1999,2003)与他的合作研究者(Glucksberg&Keysar1990,Glucksberg&McGlone1999)提出了阐释隐喻意义的范畴包容论。他们认为隐喻的本体和喻体组成临时范畴,由于没有恰当的现成词语来表达临时范畴,人们姑且以隐喻的喻体来借指上一层级的临时范畴及其特征,并把该特征归属到隐喻的本体的特征中,因此,隐喻的交际功能是双重指代功能。然而,Glucksberg等所研究的几乎都是夸张性隐喻。夸张性隐喻不仅涉及到临时范畴的构建,而且还涉及到临时语用梯级的构建。本文认为可以用推导夸张的梯级含义的方法来推导夸张性隐喻的梯级含义,即通过“下移”或“上浮”的方法,从语用梯级中的夸张程度点(或称参照点)的状况推导出语用梯级中相邻的强调程度点(或称目标点)的状况。夸张性隐喻的命题信息与背景知识的互动和张力运动使听话人从隐喻的命题所描述的事物的极限程度推导出事物的非常程度。因此,夸张性隐喻在交际中的主要功能是传递梯级含义的功能,而不是双重指代功能。

 
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