9 research outputs found
Kőzetdeformáció mechanikai és geokémiai folyamatok határán üledékes medencékben: Rock deformation at the interaction of mechanical and geochemical processes in sedimentary basins
Attesting deformation, natural fractures and faults are pervasive in low-porosity rocks in sedimentary basins. In the diagenetic realm fractures in rocks locally affect the flow of hot, reactive fluids and rock strength. Hot fluids cause dissolution, cement precipitation, and other chemical reactions, which can profoundly modify where fracture porosity, and as a consequence, connectivity exists. Although fractures may form in different settings at different locations, and at different times throughout a basin evolution history, they can potentially show similar patterns and geometric attributes, such as their position relative to bedding, shapes, aperture sizes, and cement infill types and textures. The similarity of patterns and geometric shapes impedes interpretation of intrinsically limited subsurface fracture data. Cement infills and textures, fluid inclusions trapped within, and cement isotopic compositions, on the other hand, can provide powerful evidence useful for unraveling the origin and timing of fracture formation. This presentation offers a glimpse into how geochemical analysis of fracture cements is revolutionizing fracture description and interpretation, and shows how the complexity of cement deposits are the key to unlocking the otherwise difficult-to-interpret simple patterns and geometric shapes of opening-mode fractures
MezozĂłos alkáli magmatizmus a Kárpát rĂ©giĂłban: a DitrĂłi Alkáli MasszĂvum petrogenezise = Mesozoic alkaline magmatism in Carpathian region: petrogenesis of the DitrĂł Alkaline Massif
A DitrĂłi Alkáli MasszĂvum a Keleti-Kárpátok központi kristályos kĹ‘zettömegĂ©be nyomult be, Ă©s ezekkel a metamorf kĹ‘zetekkel egyĂĽtt vett rĂ©szt az alpi tektonikai esemĂ©nyekben. Szerkezetileg a Bukovinai takarĂłhoz tartozik, annak nĂ©gy prekambriumi, kora paleozĂłos litolĂłgiai egysĂ©gĂ©vel Ă©rintkezik. A terepi (tĂ©rkĂ©pezĂ©si), petrográfiai, geokĂ©miai, izotĂłp-geokĂ©miai, cirkonmorfolĂłgiai, fluidzárvány Ă©s mikrotermometriai, raman spektroszkĂłpiai valamint kormeghatározási vizsgálatok Ă©s adatok alapján a DitrĂłi Alkáli MasszĂvum kialakulása egy kontinentális autonom magmás aktivizáciĂłhoz köthetĹ‘. A magmatizmus a kontinentális kĂ©reg kialakulása utáni, az intruzĂł a platform alapzatát átszelĹ‘ mĂ©lytörĂ©sek mentĂ©n alakult ki. Ez a magmatizmus sokfĂ©le alkáli (miaszkitos) kĹ‘zetegyĂĽttest produkált. A Tarnica Komplexum KĹ‘zetei (peridotitok, gabbrĂłk), a nefelinszienitek Ă©s gránitok közel azonos idĹ‘ben keletkezett, komagmás kĹ‘zetek. Ez a magmás tevĂ©kenysĂ©g a közĂ©psĹ‘-triász extenziĂłs tektonikai környezetben, a dĂ©l-eurĂłpai passzĂv kontinentális szegĂ©lyen, köpenyeredetű magma felemelkedĂ©sĂ©vel indult. A Bukovinai-GĂ©ta mikrokontinensnek az eurĂłpai platformtĂłl a jurában törtĂ©nĹ‘ elszakadásával, a Civcin - Severin riftrendszer mentĂ©n egy Ăşjabb, köpeny eredetű, intrĂşziĂł jött lĂ©tre. Az Ăgy keletkezett szienitek az elsĹ‘ magmás folyamat kogenetikus kĹ‘zeteivel keveredve egy sor hibrid kĹ‘zetet eredmĂ©nyeztek (dioritok, monzonitok). | The formation of the DitrĂł Alkaline Massif can be related to continental magmatic activation. The process started in the Middle Triassic at the Southern passive edge of the European continent in an extensional tectonic environment by the uplift of mantle origin magma, producing various types of petrologic associations. The rocks of the Tarnica Complex (nepheline syenites and granites) are comagmatic as they were formed almost simultaneously. By the Jurassic detachment of the Bukovina-GĂ©ta microcontinent from the European platform a new, mantle origin intrusion developed. The mixing of syenites of this formation with the rocks of the first magmatic phase resulted various hybrid rocks
Fracture, Dissolution, and Cementation Events in Ordovician Carbonate Reservoirs, Tarim Basin, NW China
Ordovician carbonate rocks of the Yijianfang Formation in the Tabei Uplift, Tarim Basin, contain deeply buried (>6000 m), highly productive oil and gas reservoirs associated with large cavities (>10 m). Previous workers inferred that large cavities are paleocaves (paleokarst) formed near the surface and subsequently buried. Alternately, caves may have formed by dissolution at depth along faults. Using 227 samples from 16 cores, we document textures and cement compositions bearing on cavity histories with petrographic, high-resolution scanning electron microscopy (SEM), isotopic, and fluid inclusion microthermometric observations. Results show that dissolution occurred at depth and was caused by (1) acidic fluids derived from Middle-Late Silurian and/or Devonian-Permian hydrocarbon generation and maturation, (2) high-temperature fluids, of which some were associated with Late Permian igneous activity, and (3) Mg-rich fluids that accompanied Jurassic-Cretaceous deformation and the formation of partially open fractures and stylobreccias (fault breccias). The relative paragenetic sequence of the structure-related diagenesis suggests seven stages of fracturing, dissolution, and cementation. Mottle fabrics in the Yijianfang Formation contain argillaceous carbonate-rich silt and are bioturbation features formed within the marine environment. Those mottled fabrics differ from clearly karstic features in the overlying Lianglitage Formation, which formed by near-surface dissolution and subsequent infilling of cavities by allochthonous sediment. Mottle fabrics are crosscut by compacted fractures filled with phreatic-vadose marine cements and followed by subsequent generations of cement-filled fractures and vugs indicating that some fractures and vugs became cement filled prior to later dissolution events. Calcite cements in fractures and vugs show progressively depleted values of δ18O documenting cement precipitation within the shallow (~220 m), intermediate (~625 m), and deep (~2000 m) diagenetic environments. Deep (mesogenetic) dissolution associated with fractures is therefore the principal source of the high porosity-permeability in the reservoir, consistent with other pieces of evidence for cavities localized near faults