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Academic literature on the topic 'Siliciclastic component'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Siliciclastic component"

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Hu, Suyun, Wenzhi Zhao, Zhaohui Xu, et al. "Applying principal component analysis to seismic attributes for interpretation of evaporite facies: Lower Triassic Jialingjiang Formation, Sichuan Basin, China." Interpretation 5, no. 4 (2017): T461—T475. http://dx.doi.org/10.1190/int-2017-0004.1.

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In China and elsewhere, it is important to predict different lithologies and lithofacies for hydrocarbon exploration in a mixed evaporite-carbonate-siliciclastic system. The lower section of the second member of the Jialingjiang Formation (T1j2L) is mainly composed of anhydrite, dolostone, limestone, and siliciclastic rocks, providing a rare opportunity to reconstruct detailed facies in a [Formula: see text] 3D seismic survey with 31 wells. Wireline logs (sonic, density, and gamma ray) calibrated by core analysis are essential in distinguishing anhydrite, siliciclastics, and carbonates. Althou

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Vernik, Lev, and Jeremy Gallop. "Elastic depth trends for siliciclastic sequences." GEOPHYSICS 87, no. 1 (2021): MR25—MR34. http://dx.doi.org/10.1190/geo2021-0137.1.

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Elastic depth trends are an integral component of reservoir characterization whether explicitly or implicitly constructed. Applications to seismic data include migration velocity model building, pore-pressure prediction, inversion, and amplitude-variation-with-offset (AVO) analysis. In practice, workflows often involve fitting well logs with smooth curves, without reference to known lithology-dependent templates that could provide realistic constraints. We have constructed porosity-depth trends for shales and sandstones with reference to reliable measurements that span mechanical compaction an

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Larsen, Michael, Brian Bell, Pierpaolo Guarnieri, Henrik Vosgerau, and Rikke Weibel. "Exploration challenges along the North Atlantic volcanic margins: the intra-volcanic sandstone play in subsurface and outcrop." Geological Society, London, Petroleum Geology Conference series 8, no. 1 (2016): 231–45. http://dx.doi.org/10.1144/pgc8.13.

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AbstractThe margins of the North Atlantic rift are covered by an extensive succession of volcanic rocks, with up to 5 km of continental flood basalts, hyaloclastites and interbedded sedimentary rocks. The volcanic succession deteriorates seismic imaging and has hampered petroleum exploration in these areas. Focused research and pioneering exploration activity, however, has improved the understanding and development of new play models in volcanic-influenced basins. In 2004, the Rosebank discovery finally proved that intra-volcanic siliciclastic sandstones of the Flett Formation may form attract

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Iannone, Antonio, Salvatore Dominech, Chaosheng Zhang, Lucia Rita Pacifico, Alessio De Falco, and Stefano Albanese. "Principal Component Analysis to Discriminate and Locate Natural and Anthropogenic Sources of Contamination Within a Strongly Anthropized Region: A Technical Workflow." Environments 12, no. 5 (2025): 163. https://doi.org/10.3390/environments12050163.

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Environmental risks often stem from contamination driven by chemical stressors introduced from multiple sources, either geogenic or anthopogenic. Differentiating between anthropogenic chemical anomalies and those inherent to the environment is crucial. This distinction is essential for defining feasible remediation objectives. This study applied univariate and multivariate statistical techniques to analyse geochemical data from over 7000 topsoil samples in Campania (Southern Italy), over an area of approximately 13,600 km2. A key step in the methodology was applying Normal Score Transformation

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Zhang, Xiangtao, Xiaoping Li, Jiayuan Du, et al. "Mixed siliciclastic-carbonate sedimentation on the Miocene Pearl River continental shelf, northeastern South China Sea: Implications for exploring lithologic traps." Interpretation 9, no. 2 (2021): SC31—SC43. http://dx.doi.org/10.1190/int-2020-0162.1.

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During the Miocene, when the Zhujiang Formation was deposited, the eastern part of the Pearl River Mouth Basin, northern South China Sea, underwent intense mixed siliciclastic and carbonate sedimentation, particularly on the platform of the marginal ramp of the Dongsha Rise, northeastern margin of the South China Sea. Cores and well logs from industrial boreholes were collected and systematically investigated to reveal the sedimentary-petrographic characteristics of the mixed deposits and their formative processes. Four lithotypes were differentiated in the deposits, that is, (1) sandstone, (2

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Putri, Shaskia Herida, Zane Jobe, Jesse Melick, Lesli Wood, and Marsha French. "Depositional-process controls on chemofacies in mixed-lithology submarine lobe deposits: a high-resolution core study from the Permian Wolfcamp XY Formation, Delaware Basin, Texas, U.S.A." Journal of Sedimentary Research 95, no. 1 (2025): 63–85. https://doi.org/10.2110/jsr.2024.015.

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ABSTRACT Mixed siliciclastic–carbonate mudrocks have variable depositional processes and diagenetic pathways, creating mineralogical complexity and thus difficulty in characterizing reservoir quality using typical subsurface datasets (e.g., well logs) as well as conventional visual core-description techniques. Core-based X-ray fluorescence (XRF) data quantifies subtle elemental variations that can aid in interpreting fine-scale sedimentological packages and variations in reservoir-property distribution. XRF data has proven to be particularly useful for interpreting and defining the depositiona

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Alsultan, Hamid, and Karrar Awad. "Sequence Stratigraphy of the Fatha Formation in Shaqlawa Area, Northern Iraq." Iraqi Geological Journal 54, no. 2F (2021): 13–21. http://dx.doi.org/10.46717/igj.54.2f.2ms-2021-12-19.

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A surface section of the Fatha Formation (Middle Miocene) was studied in the Shaqlawa area, Erbil, Northern Iraq. It consists of siliciclastic silt, evaporates, and carbonates in a mixed siliciclastic silt composition. The Fatha Formation in the study area can be divided into two members of variable thickness based on rocky differences. Depositional settings ranged from shallow open-marine and restricted-hypersaline to supratidal and continental (sabkha, fluvio-deltaic, and exposure). It is bounded below by a type one sequence boundary above the Eocene Pila Spi Formation and marked by conglome

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Georgiev, Stoyan, Valeri Sachanski, Polina Andreeva, et al. "Trans-Saharan Belt Provenance: A Potential Source for the Ordovician Succession of the Balkan Terrane (Svoge Unit) - Clues from LA-ICP-MS Detrital Zircon Dating Analysis." Proceedings of the Bulgarian Academy of Sciences 75, no. 2 (2022): 237–47. http://dx.doi.org/10.7546/crabs.2022.02.09.

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Two sandstone samples from the upper and lower part of the Ordovician succession of Svoge Unit were analyzed in order to determine their detrital zircon U–Pb age spectra using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). One sample was collected from the Hirnantian siliciclastic glaciomarine deposits of the Sirman Formation. The other sample is amiddle Darriwilian sandstone from the lower half of the Grohoten Formation. Additionally, micropetrographic studies were performed. They are composed predominantly of detrital monocrystalline quartz grains with uniform or ra

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Kiessling, Wolfgang, and Martin Aberhan. "Environmental determinants of marine benthic biodiversity dynamics through Triassic-Jurassic time." Paleobiology 33, no. 3 (2007): 414–34. http://dx.doi.org/10.1017/s0094837300026373.

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AbstractEcology is thought to be of crucial importance in determining taxonomic turnover at geological time scales, yet general links between ecology and biodiversity dynamics are still poorly explored in deep time. Here we analyze the relationships between the environmental affinities of Triassic–Jurassic marine benthic genera and their biodiversity dynamics, using a large, taxonomically vetted data set of Triassic–Jurassic taxonomic occurrences.On the basis of binomial probabilities of proportional occurrence counts, we identify environmental affinities of genera for (1) carbonate versus sil

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Kiessling, Wolfgang, and Martin Aberhan. "Environmental determinants of marine benthic biodiversity dynamics through Triassic-Jurassic time." Paleobiology 33, no. 3 (2007): 414–34. http://dx.doi.org/10.1666/06069.1.

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AbstractEcology is thought to be of crucial importance in determining taxonomic turnover at geological time scales, yet general links between ecology and biodiversity dynamics are still poorly explored in deep time. Here we analyze the relationships between the environmental affinities of Triassic–Jurassic marine benthic genera and their biodiversity dynamics, using a large, taxonomically vetted data set of Triassic–Jurassic taxonomic occurrences.On the basis of binomial probabilities of proportional occurrence counts, we identify environmental affinities of genera for (1) carbonate versus sil

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Books on the topic "Siliciclastic component"

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Argast, Scott Frederick. The hydraulic differentiation of sedimentary components and the composition and sources of Archean siliciclastic rocks from the Sargur, Javanahalli and Dharwar sequences in Karnataka, South India. 1985.

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Book chapters on the topic "Siliciclastic component"

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Pollock, Jeffrey C., Sandra M. Barr, Deanne van Rooyen, and Chris E. White. "Insights from Lu-Hf zircon isotopic data on the crustal evolution of Avalonia and Ganderia in the northern Appalachian orogen." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(08).

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ABSTRACT Avalonia and Ganderia are composite microcontinental fragments in the northern Appalachian orogen likely derived from Gondwanan sources. Avalonia includes numerous Neoproterozoic magmatic arc sequences that represent protracted and episodic subduction-related magmatism before deposition of an Ediacaran–Ordovician cover sequence of mainly siliciclastic rocks. We characterized the nature of the basement on which these arcs were constructed using zircon grains from arc-related magmatic rocks in Atlantic Canada that were analyzed for their Lu-Hf isotope composition. The majority of zircon

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Beltrán-Triviño*, Alejandro, Uwe C. Martens, and Albrecht von Quadt. "Siliciclastic provenance of the Cenozoic stratigraphic succession in the southern Gulf of Mexico: Insights from U-Pb detrital zircon geochronology and heavy minerals analysis." In Southern and Central Mexico: Basement Framework, Tectonic Evolution, and Provenance of Mesozoic–Cenozoic Basins. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2546(09).

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ABSTRACT This work presents new geochronological and mineralogical data to investigate the provenance of sediments accumulated in deep-water environments in the southern and southwestern regions of the Gulf of Mexico during the Cenozoic. We integrated U-Pb geochronology with heavy and light minerals data to better understand the provenance of the Paleocene–Miocene strata and the evolution of the sediment source terranes. The analyzed samples came from drill cuttings of sandy levels in five exploration wells offshore in the Gulf of Mexico: Puskon-1, Aktum-1, Kunah-1, Kabilil-1, and Chuktah-201.

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Wakabayashi, John. "Upper-plate versus lower-plate ophiolitic assemblages and their significance in interpreting orogenic belt evolution and processes." In The Virtue of Fieldwork in Volcanology, Sedimentology, Structural Geology, and Tectonics—Celebrating the Career of Cathy Busby. Geological Society of America, 2025. https://doi.org/10.1130/2025.2563(18).

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ABSTRACT Ophiolitic rocks occupy different positions relative to paleosubduction zones and have a variety of origins. Distinguishing the structural-tectonic positions of such ophiolitic assemblages is important for relating the ophiolitic rocks to tectonic processes and orogenic history. The California Coast Ranges facilitate recognition of the original structural-tectonic setting of the ophiolitic rocks in the area because the subduction episode associated with them terminated by conversion to a transform plate margin, rather than continental collision, and exhumation since subduction termina

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Conference papers on the topic "Siliciclastic component"

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Wijaya, A. K. "The Significant Impact of Intraformational Seal to Hydrocarbon Accumulation of Mixed Carbonate - Siliciclastic Sequences In Oligo-Miocene Interval, North Madura Platform, East Java Basin." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-g-480.

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The major reservoir within the North Madura Platform is the Oligo-Miocene Interval, which consists of oil and gas-bearing reservoirs, with multiple reservoir layers and multiple hydrocarbon contacts. The interval comprises of a stacked high frequency cycles of mixed carbonate-siliciclastic lithology component sitting in the paleo-high. It has become very important in the context of hydrocarbon accumulation since the components play very dissimilar roles and become reservoir-seal pairs, which resulted in the existence of intraformational seal. Based on the carbonate to siliciclastic ratio, from

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Haines, PW, H. J. Allen, MTD Wingate, LS Normore, Y. Lu, and IOH Fielding. "The Murraba Basin revisited – interpretations refined by detrital zircon data." In Central Australian Basins Symposium IV. PESA, 2024. http://dx.doi.org/10.36404/ggor3006.

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The Murraba Basin is a poorly known component of the Centralian Superbasin that extends across the Western Australia – Northern Territory border. An earlier reconnaissance reinterpretation by some of the authors significantly changed the inferred ages and order of stratigraphic units and demonstrated many similarities to the Neoproterozoic and lower Cambrian component of the nearby, and presumably contiguous, Amadeus Basin. Further refinements are now possible with the addition of detrital zircon geochronology of siliciclastic units in the area. Detrital zircon data show that the Hidden Basin

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Sinha, Supriya, Karol Riofrio, Arthur Walmsley, Nigel Clegg, Stig Sviland-Østre, and Nicolas Gueze. "REAL-TIME 3D IMAGING OF COMPLEX TURBIDITIC RESERVOIR ARCHITECTURE." In 2021 SPWLA 62nd Annual Logging Symposium Online. Society of Petrophysicists and Well Log Analysts, 2021. http://dx.doi.org/10.30632/spwla-2021-0041.

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Siliciclastic turbidite lobes and channels are known to exhibit varying degrees of architectural complexity. Understanding the elements that contribute to this complexity is the key to optimizing drilling targets, completions designs and long-term production. Several methods for 3D reservoir modelling based on seismic and electromagnetic (EM) data are available that are often complemented with outcrop, core and well log data studies. This paper explores an ultra-deep 3D EM inversion process during real-time drilling and how it can enhance the reservoir understanding beyond the existing approac

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Cheng, L., B. R. Crawford, H. Chen, J. H. Macquaker, and D. McLendon. "Mechanical Upscaling in Highly Heterogeneous Rock Masses: Impact on Anisotropy and Subsurface Stress Prediction in the Bone Spring and Wolfcamp Formations of the Delaware Basin, USA." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0473.

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ABSTRACT: The unconventional Bone Spring and Wolfcamp Formations are the development focus in the Delaware Basin. However, the high heterogeneity of the reservoir rocks challenges the selection of landing zones and increases the uncertainty of well performance. Estimating faithful elastic properties and predicting stress profiles along the wellbores are key to improve production and stimulation design. We acquire over 3,000 feet of continuous cores from five wells in New Mexico, Delaware Basin. We combine a variety of high-resolution, whole core-based characterization techniques that include h

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Sapiie, B. "Fault Seal Analysis Application in Carbonate Rock Sequences: Issues and Solution." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-g-303.

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Fault seal analysis (FSA) is a crucial component of hydrocarbon exploration, production, and reservoir management. However, most FSA workflow and theories are developed for normal fault systems that commonly apply to siliciclastic rock. In the case of the carbonate rock, a simple algorithm of FSA using shale gouge ratio (SGR) analysis may generate some errors in sealing and leaking faults. The FSA method is primarily controlled by shale volume distributions rather than by throw, as demonstrated by sealing faults behavior with small throws. This result suggested that good quality sand reservoir

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Wuryanto, Argo, Wilsen Supriady Lauwijaya, Thomas Yunanto Yoga, et al. "Unleashing the Potential of Siliciclastic Reservoirs in the Sepinggan Carbonate Sequences, A Discovery in the South Mahakam Field, Lower Kutai Basin." In SPE/IATMI Asia Pacific Oil & Gas Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/215417-ms.

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Abstract The M-1x exploration well has successfully identified substantial hydrocarbon discoveries within the Sepinggan Deltaic Sequences (SDS) and Sepinggan Carbonate Sequences (SCS). However, investigating siliciclastic reservoirs in the shallow part of the SCS in the Mahakam PSC has been hindered by challenges associated with carbonate intervals. In this study, recent seismic reprocessing data is utilized to enhance structural predictions and reservoir characterizations, providing valuable insights for future well development. A comprehensive suite of logging acquisitions, including pressur

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Sahu, Pallavi Sahu, and Zoya Heidari. "Assessment of Petrophysical Heterogeneity Based on Image Data." In 2024 SPWLA 65th Annual Symposium. Society of Petrophysicists and Well Log Analysts, 2024. https://doi.org/10.30632/spwla-2024-0058.

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Formation heterogeneity that broadly defines the spatial variations in rock properties has long been recognized as an important factor for the reliable assessment of petrophysical properties and their variation in subsurface rocks. Conventional methods to quantify formation heterogeneity depend on visual inspection of core samples or statistically derived well-log-based coefficients. These coefficients represent heterogeneity in a data set by a single value and overlook discontinuity in petrophysical properties. To fully understand the depth-by-depth variability in petrophysical properties, it

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Nebelsick, James. "BIOSEDIMENTATION IN MIXED CARBONATE-SILICICLASTICS: USING COMPONENT ANALYSIS AND MICROTAPHOFACIES TO ANALYZE DEPOSITIONAL ENVIRONMENTS OF THE NORTH ALPINE FORELAND BASIN." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357706.

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Magnall, Joseph M., and Sarah A. Gleeson. "Fraternal twins or distant cousins; comparing and contrasting the Red Dog district and Irish Midlands Orefield." In Irish-type Zn-Pb deposits around the world. Irish Association for Economic Geology, 2023. http://dx.doi.org/10.61153/ifmh3823.

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The Lower Carboniferous rocks in the Irish Orefield and Red Dog district are host to some of the highest value Zn deposits in the geological record. A comparison of different mineral system components (geodynamic setting, (basin) architecture, fluid flow drivers, and depositional mechanisms) between the two districts reveals there are perhaps more similarities than differences. These include the complex accretionary evolution of the underlying basement terranes, ore fluid chemistry, common age of the mineralization for some of the deposits (331 – 346Ma), timing of mineralization relative to ho

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Catianis, Irina, Adriana Maria Constantinescu, Dan-Lucian Vasiliu, Bogdan-Adrian Ispas, and Dumitru Grosu. "PHYSICAL AND CHEMICAL CHARACTERISTICS OF TATARU AND MERHEI LACUSTRINE SEDIMENTS, FROM THE DANUBE DELTA, ROMANIA." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/5.1/s20.042.

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The quality and quantity of delta lakes� sediment depend on fluvial input and in-situ bio-geo-chemical processes. The present study investigates the quality of lacustrine sediments collected from two lakes - Tataru and Merhei, situated in different hydrodynamic environments within the Danube Delta, Romania, but both connected to fluvial input of water and sediment of the Danube. The following physical and chemical analyses have been carried out on several lake-bottom sediment samples: the main lithological components (total organic matter-TOM%, total carbonates-CAR% and siliciclastic fraction-

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