Morphostructural investigation within the Orihovo-Pavlograd zone

Z. Tovstyuk, T. Yefimenko
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Abstract

This detailed investigation was conducted for the South part of the Orikhovo-Pavlograd suture zone by using satellite imagery. At the first stage, the imagery was used to extract lineaments and arcuate relief elements. Further, geomorphological anomalies were highlighted by means of structural and geomorphological analysis of the study area.  The significant number of ultrabasite bodies were distinguished alongside the entire Orikhovo-Pavlograd suture zone with allowance for the geological structure. The sites of kimberlite magmatism defined according to geophysical investigations can be associated with ultrabasite bodies. Prognostic sites of kimberlite magmatism were allocated and complex of morphostructural geoindication features were educed above the prognostic paleo-volcano that had erupted ultrabasites. The geoindicators of morphostructures are: the spreading and narrowing of a floodplain; displacement of a stream bed; deeping of the stream bed plunging depth; straightened reach of the stream bed; discordant course of the left tributaries of the Molochna river; augmentation of the stream bed meandering; floodplain marshy parts at the beginning of morphostructures; intense developing of a ravine-gully network on the right side of the Molochna river; localization of sand massifs on the anomalously located second terrace of the Molochna river flood-plain; rills and numerous artesian wells within the floodplain. These indicators have made it possible to construct a geoindication scheme, distinguish the prognostic Melitopol morphostructure and make a prognosis for mineral exploration. The formation of this morphological structure can be ascribed with a paleo-volcano, which igneous rocks are ultrabasites and kimberlites. Rocks of these complexes can be prospective evidence for diamond, iron, nickel, copper, lead and zinc deposits exploration. Hydrothermal and metasomatic sulphide (polymetallic) mineral occurrences can be explored as well. The procedure of geoindication investigation will be applied for integrated exploration throughout the entire area of the Orekhovo-Pavlograd suture zone.
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Orihovo-Pavlograd区的形态结构调查
利用卫星图像对Orikhovo-Pavlograd缝合带的南部进行了详细的调查。在第一阶段,使用图像提取轮廓和弓形浮雕元素。通过构造和地貌分析,突出了研究区地貌异常。在考虑到地质构造的情况下,在整个Orikhovo-Pavlograd缝合带附近发现了大量的超基岩体。根据地球物理调查确定的金伯利岩岩浆活动的位置可以与超基岩体联系起来。在曾喷发过超基岩的预测古火山上方,划分了金伯利岩岩浆活动的预测位点,导出了复杂的形态构造地质指示特征。形态构造的地理标志是:河漫滩的扩展和缩小;河床位移;河床的纵深;河床的伸直段;莫洛契纳河左支流的不和谐河道;加强河床曲流;漫滩沼泽部分初期形态构造;莫洛契纳河右侧形成了强烈的沟壑网;莫洛契纳河冲积平原第二阶地异常位置的砂体定位;河漫滩内的小溪和众多自流井。这些指标为构造地质指示方案、鉴别预测地貌、进行找矿预测提供了可能。该形态结构的形成可归因于古火山,火成岩为超基岩和金伯利岩。这些杂岩体可作为寻找金刚石、铁、镍、铜、铅、锌矿的远景证据。热液和交代硫化物(多金属)矿床也可勘探。在整个Orekhovo-Pavlograd缝合带地区,将采用地理标志调查程序进行综合勘探。
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