A hydrocarbon column Ultradeep wells was built and the presence and content of hydrocarbons in different ages and genetic types of rocks was traced. Ultradeep Kola depth of 12,262 meters in Archean, Proterozoic crystalline schists, granites , gneisses etc., Ultradeep Bertha Rogers depth of 9583 meters in Paleozoic shale , sandstone, limestone etc., Ultradeep Saatli 8268 meters in, Mesozoic, Cenozoic sedimentary, basalt rocks. So in analyze involve common depth from 0, 0 to 12,262 meters and different genetic type of rocks-sediments, magmatic, metamorphic. On the all profile Ultradeep wells, Hydrocarbons is represented by the entire spectrum: light (CH 4 ), heavy (HHC), normal, isoforms, saturated, non-saturated etc. Hydrocarbons of the same composition are present in genetically different antagonistic types of rocks and of different ages, making up the Hydrocarbon Temporal-Facial Continuum of the Earth's Crust. Despite genetically different antagonistic types of rocks, they generate the same common-united HC, which can be said that HC are generated by various processes -sedimentary, magmatic, metamorphic, making up the Hydrocarbon heterogeneous continuum of the Earth's Crust. It should be noted that the Kola borehole did not reveal a basalt layer, and according to 1 layer Model of the Earth's Crust Galant (MECG), (AAPG Athens 2007, EGU. Vienna 2013), the granites of the Earth's Crust of the continents are distributed up to the mantle. Interpolating the presence of hydrocarbons from the bottom of the Kola well into the depths, it is expected that the entire Earth's crust of the continents up to the mantle is saturated with Hydrocarbons! Hydrocarbons Ultradepth can be a source of oil and gas fields.
<p>Searching for oil in Germany is an urgent task, since from its own reserves Germany can cover only four percent of the total volume of oil required for the country's economy. In this regard, we have conducted research with the aim of assessing the prospects of the Rhine Rift oil potential. Were analyzed in basalts Polycyclic Aromatic Hydrocarbons (PAH). The PAH Petroleum Association clearly indicates the presence of petroleum hydrocarbons in rocks and are an indicator of the oil content of deep horizons. The previous report (EGU2020) highlighted the positive factors of oil&#160;&#160; potential in the Rhine Rift. There are favorable geological settings of Rhine Rift, such as seismic activity, new tectonic movements, and presence of basalt, decompressed rocks of mantle, rift stretching mode, and favorable geochemical indications, such as existence of typomorphic oil-associated PAH (Phenanthrene, Chrysene, Pyrene, Benz(a)pyren), presence the components resembling on compositions of Moravia oil . For detailing research conducted mathematical correlation between the non-hydrocarbon components PAH (Naftalen + Homologus, Difenil, Benz (ghi) perylene, Fluorene, Perilen, Antracen, Tetraphen) and hydrocarbon components PAH (Phenanthrene, Pyrene, Chrysene, Benz(a)pyren). Mathematical correlation is 0.041, which is a weak positive relationship on the Chaddock scale. The weak positive relationship between the oil components of PAHs and non-oil components probably indicates that the sources of the oil components of PAHs and non-oil components of PAHs are different. And the source of the oil PAHs is probably the oil fields. Thus the geological-geochemical-mathematical factors point to favorable oil-bearing entrails Rhine Rift<strong>!</strong> For prospecting&#160;&#160; cluster of oil&#160;&#160; in the first instance recommended at areas: Bad Urah, Kaizertuhl-Shellingen <strong>!</strong></p><p>&#160;</p>
The present paper highlights the problem related to the source of hydrocarbons in the Eger Rift in Czech Republic. The authors discuss the existence of polygenetic deep sources of hydrocarbons. The investigations are based on direct indicators of Polycyclic Aromatic Hydrocarbons (abbr. PAHs). Among the diverse components of PAHs has been recognized typomorphic oil association -videlicet: phenanthrene, chrysene, pyrene and benzo(a)pyrene. On the basis of new geochemical, geological and mathematical data the oil and gas potential of Eger Rift is also discussed.
<p>For the formation of oil (PG), a certain geological and geochemical environment of the Earth's Crust is necessary. Geologically, the current PG models are based on a 2-layer model of the Earth's Crust, consisting of Granite and Basalt layers. However, as the drilling of the Kola Superdeep Borehole (SG3) showed, there is no basalt layer on the continents. A model of a 1-layer Earth's Crust was compiled, consisting of a granite layer on the continents and a basalt layer in the Oceans:[1 layer&#160; &#1052;odel of the Earth's Crust Galant (MECG), ( AAPG, Athens 2007; EGU, Vienna 2013,2022;)] &#1089;onsist of separated layers of &#160;Granite &#160;and separated layers of &#160;Basalt. This Model of the Earth's Crust Galant (MECG) fundamentally changes the geological and geochemical setting of the Earth's Crust and hence the PG processes. Basalts and Granites are antipodes and therefore fluids migrating from the mantle with the goal of generating oil passing through the Earth's Crust that does not have Basalts but has only Granites will behave differently - respectively. In connection with the change in the geological and geochemical situation, the parameters of the fluid migrating from the mantle will also change: the C-O-H ratio, reactions with the components of the layer, the supply and removal of components, the change in T, the intensity of degassing, the change in the fugacity of O, the depth of the depleted mantle, etc. Since the Kola on the Baltic Shield did not reveal the basalt layer and due to this, the depth [According based on 1 layer Model of the Earth's Crust Galant (MECG), ( AAPG Athens 2007, EGU Vienna 2013)] of the granite layer reaches the mantle deeply and the greater the thickness the thickness of the depleted mantle is greater, from this it can be assumed that the mantle gave up light hydrocarbon components concentrated in the upper horizons of the Lithosphere, and heavy hydrocarbon components still remained in the depleted mantle or are now slowly migrating upward into the granite layer. This may explain that granites contain more light hydrocarbons. Due to the change in the physical and chemical conditions of the Earth's Crust, the PG depth zone changes, expands or localizes, and the composition of the oil changes accordingly. CONCLUSIONS: In connection with the 1-layer model of the Earth's Crust, the energy-material exchange between the domains of the Earth, the Mantle and the Lithosphere changes. Characteristics of the parameters of physic-chemical conditions change. And also the tactics, strategy, philosophy of PG research should change, taking into account the new model of the Earth's Crust.</p> <p>&#160;</p>
<p>&#160;</p><p>Earlier (GeoBio 2014, Moscow ) it was reported that an independent domain is observed in the Earth's &#1057;rust - the Hydrocarbon Sphere (HCS). HCS is a sequential alternation of hydrocarbon fields in accordance with geological objects. HCS is a material space-time continuum spread throughout Earth Crust, from Archean to modern precipitation. On the scale of the Earth's crust, HCS is represented by the entire HC spectrum (light CH<strong><sub>4</sub></strong>, heavy HHC, normal, isoforms, etc.). Globally, chemically, the HCS gas composition of the Earth's Crust of the granite layer is similar to the HCS composition of gas fields and is equal to CH<strong><sub>4</sub></strong>-HHC, while the basalt layer corresponds to the HCS composition of oil fields and is equal to HHC - CH<strong><sub>4</sub></strong>. Structure of HCS&#160;&#160; of the Earth Crust based on 1 layer&#160; &#1052;odel of the Earth's Crust Galant (MECG), ( AAPG Athens 2007, EGU Vienna 2013) &#1089;onsist of separated layers of CH<strong><sub>4</sub></strong>-HHC (Granite HC Sphere)and separated layers of HHC - CH<strong><sub>4</sub></strong> (Basalt HC Sphere ).&#160;&#160; Considering that, according to the MECG model, &#8220;there is no basalt crust under the granite crust, and there is no granite crust under the basalt crust&#8221;, both HCS<strong> </strong>of the Earth's Crust - Granite HC Sphere and Bazalt HC Sphere lies directly on mantle.</p><p>&#160;</p>
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