FACIAL-PALEOGEOGRAPHIC RECONSTRUCTIONS OF THE VALANGINIAN-HAUTERIVIAN STRATA BELONGING TO THE LOWER CRETACEOUS GYDAN PENINSULA AND THE WESTERN PART OF THE YENISEI-KHATANGA REGIONAL FOREDEEP

N. Taninskaya, V. V. Shimanskiy, N.Ya. Raevskaya, N.Ya. Vasil'ev, I. Nizyaeva, M.V. Nugumanova, M. Birin, I. Gizdatullina
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Abstract

Paleogeographic reconstructions were carried out, sedimentation models were determined, and facies-paleogeographic maps were constructed for the Valanginian-Hauterivian clinoform structures of the Lower Cretaceous of the Gydan Peninsula and the western part of the Yenisei-Khatanga foredeep based on the facies interpretation of the core, well logging and using seismic data. Revealed sedimentation criteria for the development of reservoir rocks. The distribution of rocks with improved reservoir properties is confined to the zones of development of facies of river channel shoals, accumulative sandy bodies of the coastal-marine zone, delta channels, delta fans and turbidites.
格旦半岛和叶尼塞-哈坦加区域前深西部下白垩统瓦兰吉尼亚-豪特里维亚地层的面相古地理重建
在岩心相解释、测井资料和地震资料的基础上,对吉丹半岛下白垩统瓦兰吉尼亚-豪特里维亚斜形构造和叶尼塞-哈坦加前深西部进行了古地理重建,确定了沉积模式,绘制了相古地理图。揭示了储层发育的沉积标志。储层物性较好的岩石主要分布在河道滩相发育带、滨海带堆积砂体相发育带、三角洲河道相发育带、三角洲扇相发育带和浊积岩相发育带。
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