盐丘周围高产岩的类似物清单

Valentyn Loktyev, Sanzhar Zharkeshov, O. Hotsynets, O. Davydenko, M. Machuzhak, Kuzmenko Pavlo, V. Repryntsev
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摘要

在第聂伯-顿涅茨洼地,石炭纪时期的泥盆纪盐变得可移动,并在二叠纪时期形成了盐丘,向海底移动并随之流动,形成了今天可见的盐冠层和悬垂物。这些特征是地表盐暴露的清晰证据,特别是考虑到盐丘周围的储层带。这些储层在某些井中可能非常多产。之前针对此类矿床的勘探主要是通过在已知的深层油田(如Medvedivske、Zakhidno-Khrestyschenske和DDB中部的其他地区)钻探井来驱动的。这些储层由各种岩石的粗糙物质组成,包括砂岩、碳酸盐岩、白云岩、深部(花岗岩)和浅层(辉绿岩)地层的火成岩。目前,随着三维地震勘探的可用性,这些沉积物可以被发现为亮点和平坦点。虽然它不是一个100%的指标,因为浅盐层和盐丘周围岩石的岩性变化也可能解释地震反射。值得一提的是,二叠纪是一个干旱的环境,在1-2公里的厚度范围内,从底部到顶部逐渐失去水流入盆地。它可以用作边界类比物,以涵盖三个领域的大多数可能的中间情景。第一个类似的例子是位于乌克兰西部靠近罗马尼亚边境的喀尔巴阡山脉的Solotvyno村的露头盐丘。这个盐丘是一个重要的例子,展示了从盐丘周围深处运输的粗质物质的当前沉积。第二个是像阿曼沙漠山脉一样暴露的盐丘,在那里可以沿着物质路径接近盐隆起。第三个例子是美国亚利桑那州的死亡谷。这个山谷就是一个扇形的例子,大部分是由重力而不是永久的水流沉积的。值得一提的是,还有更多的例子可以被视为直接的类似物(伊朗的扎格罗斯山脉),但如果需要的话,它们不容易进行实地考察。为了识别真实目标与人工制品,应用世界各地当前沉积案例的知识将会有很大帮助(西乌克兰、阿曼、亚利桑那州的死亡谷)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
List of Analogues for Highly Productive Rocks Around Salt Domes
In the Dnipro-Donets depression, the Devonian salt during Carboniferous time became movable and created salt domes in the Permian, moving to the sea bottom and flowing therewith, forming bodies visible today as salt canopies and overhangs. These features are clear pieces of evidence of salt exposure on the surface, especially considering belts of reservoirs around salt domes. These reservoirs can be extremely prolific in some wells. Previous exploration targeting such deposits was driven mainly by drilling wells within the areas of known deep fields such as Medvedivske, Zakhidno-Khrestyschenske and others in the central part of the DDB. These reservoirs are composed of poorly sorted coarse material of wide variety of rocks including sandstones, carbonates, dolomites, igneous rocks of deep (granites), and shallow (diabases) formations. Currently, with the availability of 3D seismic surveys, these deposits become visible as bright spots and flat spots. Although it is not a 100% indicator due to fact that shallow salt canopies and lithology changes of rocks around salt domes may also interpret seismic reflections. It is good to mention that the Permian is an aridic environment with gradually losing water influx to the basin from base to top within the thickness of more than 1-2 kilometers. It could be utilized as boundary analogues to cover most of the possible intermediate scenarios in three areas. The first analogue is the outcropped salt dome in Solotvyno village in Carpathian mountains in western Ukraine close to the Romania border. This salt dome is an important example of showing the current deposition of transported coarse material from depth around salt domes. The second one is salt domes exposed as mountains of the Oman desert where it is possible to follow the material path approaching the salt uplift. And the third example is the Death Valley in Arizona, USA. The valley is an example of fans mostly deposited by gravity rather than permanent water flows. It good to mention that there are more examples that could be treated as direct analogues (the Zagros mountains in Iran) but they are not easily accessible for field trips if needed. For recognizing real targets vs artifacts, applying the knowledge of current deposition examples around the world would help dramatically (Western Ukraine, Oman, Death Valley in Arizona).
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