№ 5 (2024)

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Articles

Late Cretaceous Okhotsk-Penzhina-Anadyr Small Oceanic Basin (Northeast Eurasia): Geological Evidence and Geodynamic Evolution

Chekhovich V., Palandzhyan S.

Аннотация

The modern structure of the Eurasian Margin combines supra-subduction Upper Cretaceous volcanogenic formations – the marginal continental Okhotsk-Chukchi volcanogenic belt and the accreted Nemuro‒Olyutor intra-oceanic arc formed during the subduction of the oceanic crust of the Pacific. We consider the formation of the Okhotsk-Chukchi volcanic belt, separated by the Nemuro-Olyutor intraoceanic arc from the Pacific, in the conditions of a paleo-oceanic basin that existed for ~20 Ma. As a result of the conducted paleo-geodynamic analysis, it was found that in the Late Cretaceous in northeastern Eurasia, between the Eurasian continent and the tectonic blocks of the Sea of Okhotsk, Western Kamchatka, and Northern Koryak located to the south and southeast of it, a small oceanic basin of the pull-apart type developed in the conditions of transtension, which can be called the Okhotsk‒Penzhina‒Anadyr. This basin was formed as a result of a major strike slip fault when terranes tectonic escaped out of the eastern part of the closing Mongol‒Okhotsk Ocean. The progressive opening of the Okhotsk‒Penzhina‒Anadyr spreading basin subducted from the southwest to the northeast under the Eurasian continent, which caused a corresponding delay in the onset of supra-subduction volcanism in the Okhotsk‒Chukchi Belt. The geodynamic evolution of the southwestern and northeastern parts of the Okhotsk‒Penzhina‒Anadyr basin differed in that the Iruney (West Kamchatka) island arc arose and developed in the southwestern part of it, earlier in time of formation, near the West Kamchatka continental block. In the northeast, the arc was bounded by a transform fault that stretched to the southeast, delimiting not only the Kamchatka terrane from the North Koryak and Uchkhichkhil, but also the Valaginsky (East Kamchatka) and Olyutor intra-oceanic island arcs. In the Cenozoic stage of development, this fault was transformed into the Palano‒Ozernovskaya trans-litospheric zone, which is the boundary between the accreted Olyutor and East Kamchatka terranes of the Nemuro-Olyutor island arc system. A geodynamic model of the pre-arc, the Alb‒Turonian stage of intra-oceanic subduction, which lasted until the beginning of the formation of the early Nemuro arc in the coniacian, was applied the Olyutor island arc system. The duration of the pre-arc stage of intra-oceanic subduction corresponds to the time of the same stage of the geodynamic evolution of Izu‒Bonin‒Mariana Island arc system. This allows us to confirm the expansion of Pacific since the Albian time due to subduction in Nemuro‒Olyutor island-arc system.

Геотектоника. 2024;(5):3-27
pages 3-27 views

Structural Connection of the Chukchi Borderland and the Chukchi Sea Shelf: 3D Geophysical Modelling of the Earth Crust

Piskarev A., Kireev A., Ovanesyan G., Poselov V., Savin V., Smirnov O., Tabyrtsa S.

Аннотация

A 3D model of the crustal structure of the region, which includes the Chukchi Borderland with the adjacent ocean and the Chukotka‒Alaska Shelf, has been compiled and calculated. The peculiarity of the crustal structure is the three-sided isolation of the Chukchi Borderland and presence of a transitional area from the south connecting the Chukchi Borderland with the Chukotka‒Alaska Shelf. The connection between the Chukchi Borderland and the Wrangel Rise of the Chukchi Shelf is traced through the North Chukchi Rise located between the North Chukchi Trough and the Hanna Trough. A clockwise rotation of the Chukchi Borderland began in the Early Cretaceous, because basalts at the bottom of the sedimentary strata sections along the eastern and southern boundaries of the Chukchi Basin have a reversed magnetization, i.e., their outpouring occurred before the beginning of the Cretaceous superchron, earlier than 121 Ma. Near the upper boundary of the Neocomian, there was a large-scale shear displacement of crustal blocks along the eastern boundary of the Chukchi Rise, which had a thrust pattern before that. The 3D model demonstrates that the Chukchi Borderland and the Chukchi Basin are the natural components of the continental margin, as they have a strong geological connection with the continental masses of the Chukchi Shelf.

Геотектоника. 2024;(5):28-45
pages 28-45 views

Geology and Hydrocarbon Potential of the Subsalt Deposits of the Astrakhan Arch in the Caspian Petroleum Province: Results of Comprehensive Study

Volozh Y., Abukova L., Antipov M., Komarov A., Merkulov O., Patina I., Rybalchenko V., Soin D., Titarenko I.

Аннотация

The article summarizes the results of the authors’ work on the comprehensive substantiation of the geological, tectonic, and geofluid-dynamic conditions for generating and accumulation of hydrocarbons in the subsalt floor of the Astrakhan Arch inside the Caspian oil and gas Province.

We analyzed a significant amount of archival geological and geophysical data and materials such as (i) an array of regional seismic profiles; (ii) gravity and magnetic exploration data of different scales; (iii) results of deep drilling.

Specific seismic geological bodies that are capable of serving as oil and gas reservoirs have been identified. For the first time in creating the geological model of the Astrakhan Arch, its location within the autoclave hydrocarbon system of the subsalt floor of the Central subprovince of the Caspian oil and gas Province (within the Astrakhan-Jambay oil and gas accumulation zone) has been taken into account. This allowed the authors to substantiate the geofluid dynamic nature of the number of large non-structural-type oil and gas reservoirs boundaries. It is opening up new possibilities for predicting oil and gas fields, including those with low sulfur content. Several generation-accumulation mini-hotbeds have been identified on the Astrakhan Arch, and in three of them - reservoirs with increased probability of discovering oil and gas fields. The main result of the study is the refinement of the initial total geological resources of hydrocarbons of the Astrakhan Arch and adjacent areas.

Геотектоника. 2024;(5):46-68
pages 46-68 views

Structure of Salt Diapirs in the Western Siberian Basin and Yenisei‒Khatanga Trough Based on Seismic Data

Sobornov K.

Аннотация

Interpretation of regional seismic profiles characterizing the structure of the West Siberian basin and the Yenisei-Khatanga Trough to depths of 10‒20 km suggests that salt diapirs played an important role in the structure of this region. Salt diapirs have the following features: (i) large height (up to 5 km or more); (ii) seismic transparency; (iii) presence of growth layers on the flanks of inferred salt rises; (iv) existence of radial fault systems in overlying sediments; (v) isometric shapes of uplifts; (vi) reduced values of the gravity field. Salt deformation explains the origin of widespread ring inversion structures in Jurassic-Cretaceous sediments. Such ring structures probably originated above long-lived salt diapirs. The salts in them are presumably of Early Paleozoic age. The formation of salt strata took place in a large area of salt accumulation at the periphery of the Siberian Platform. The western boundary of the zone of evaporitic sediments distribution is the Trans-Eurasian fault zone, which separated the folded Uralides from the Siberian Platform and tectonic blocks amalgamated with it. The presence of the evaporitic Paleozoic deposits in the northeast of the West Siberian Basin and the Yenisei-Khatanga Trough facilitated the development of large oil and gas pools. Salt cryptodiapirs focused the migration of hydrocarbons from deeply buried, thermally mature Paleozoic sediments into the Jurassic-Cretaceous section, which explains the predominance of gas deposits in these areas, as well as the multilayer nature of the fields.

Геотектоника. 2024;(5):69-94
pages 69-94 views