Relevant bibliographies by topics / Paleo Channel system

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Paleo Channel system'

Author: Grafiati
Published: 23 September 2021
Last updated: 18 July 2025

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Journal articles on the topic "Paleo Channel system"

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Hassenruck-Gudipati, Hima J., Thaddeus Ellis, Timothy A. Goudge, and David Mohrig. "A multi-proxy assessment of terrace formation in the lower Trinity River valley, Texas." Earth Surface Dynamics 10, no. 3 (2022): 635–51. http://dx.doi.org/10.5194/esurf-10-635-2022.

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Abstract. A proposed null hypothesis for fluvial terrace formation is that internally generated or autogenic processes, such as lateral migration and river-bend cutoff, produce variabilities in channel incision that lead to the abandonment of floodplain segments as terraces. Alternatively, fluvial terraces have the potential to record past environmental changes from external forcings that include temporal changes in sea level and hydroclimate. Terraces in the Trinity River valley have been previously characterized as Deweyville groups and interpreted to record episodic cut and fill during late
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Bellwald, B., S. Planke, S. Polteau, et al. "Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjørnelva River Valley, SW Barents Sea." Journal of Glaciology 67, no. 263 (2021): 404–20. http://dx.doi.org/10.1017/jog.2020.115.

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AbstractProglacial braided river systems discharge large volumes of meltwater from ice sheets and transport coarse-grained sediments from the glaciated areas to the oceans. Here, we test the hypothesis if high-energy hydrological events can leave distinctive signatures in the sedimentary record of braided river systems. We characterize the morphology and infer a mode of formation of a 25 km long and 1–3 km wide Early Pleistocene incised valley recently imaged in 3-D seismic data in the Hoop area, SW Barents Sea. The fluvial system, named Bjørnelva River Valley, carved 20 m deep channels into L
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de Weger, Wouter, F. Javier Hernández-Molina, Rachel Flecker, et al. "Late Miocene contourite channel system reveals intermittent overflow behavior." Geology 48, no. 12 (2020): 1194–99. http://dx.doi.org/10.1130/g47944.1.

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Abstract Paleoceanographic information from submarine overflows in the vicinity of oceanic gateways is of major importance for resolving the role of ocean circulation in modulating Earth’s climate. Earth system models are currently the favored way to study the impact of gateways on global-scale processes, but studies on overflow-related deposits are more suitable to understand the detailed changes. Such deposits, however, had not yet been documented in outcrop. Here, we present a unique late Miocene contourite channel system from the Rifian Corridor (Morocco) related to the initiation of Medit
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Bukar, Shettima, Mohammed Bukar, Asabe Kuku, Bintu Shettima, and Ishaku H. Kamale. "Incised Valley Depositional System of the Cretaceous Yolde Formation of the Gongola Sub-basin Northern Benue Trough N.E. Nigeria." European Journal of Engineering Research and Science 5, no. 8 (2020): 870–76. http://dx.doi.org/10.24018/ejers.2020.5.8.1999.

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This research was carried out in the Gongola Sub-basin of the Northern Benue Trough aimed at deciphering of the paleo-depositional environment of the Yolde Formation based on facies on facies analysis. Six lithofacies were identified to include trough crossbedded sandstone facies (St), massive bedded sandstone facies (Sm), planar crossbedded sandstone facies (Sp), ripple laminated sandstone facies (Sr), parallel sandstone facies (Sl) and mudstone facies (Fm). These build into two facies association of fluvial channel and tidally influenced fluvial channel facies associations. The fluvial succe
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Bukar, Shettima, Mohammed Bukar, Asabe Kuku, Bintu Shettima, and Ishaku H. Kamale. "Incised Valley Depositional System of the Cretaceous Yolde Formation of the Gongola Sub-basin Northern Benue Trough N.E. Nigeria." European Journal of Engineering and Technology Research 5, no. 8 (2020): 870–76. http://dx.doi.org/10.24018/ejeng.2020.5.8.1999.

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This research was carried out in the Gongola Sub-basin of the Northern Benue Trough aimed at deciphering of the paleo-depositional environment of the Yolde Formation based on facies on facies analysis. Six lithofacies were identified to include trough crossbedded sandstone facies (St), massive bedded sandstone facies (Sm), planar crossbedded sandstone facies (Sp), ripple laminated sandstone facies (Sr), parallel sandstone facies (Sl) and mudstone facies (Fm). These build into two facies association of fluvial channel and tidally influenced fluvial channel facies associations. The fluvial succe
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Pelletier, J. D. "The linkage between hillslope vegetation changes and late-Quaternary fluvial-system aggradation in the Mojave Desert revisited." Earth Surface Dynamics Discussions 2, no. 1 (2014): 181–213. http://dx.doi.org/10.5194/esurfd-2-181-2014.

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Abstract. Valley-floor-channel and alluvial-fan deposits and terraces in the southwestern US record multiple episodes of late Quaternary fluvial aggradation and incision. Perhaps the most well constrained of these episodes took place from the latest Pleistocene to the present in the Mojave Desert. One hypothesis for this episode, i.e. the paleo-vegetation change hypothesis (PVCH), posits that a reduction in hillslope vegetation cover associated with the transition from Pleistocene woodlands to Holocene desert scrub generated a pulse of sediment that triggered a primary phase of aggradation dow
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Bindi, L., F. Tasselli, F. Olmi, A. Peccerillo, and S. Menchetti. "Crystal chemistry of clinopyroxenes from Linosa Volcano, Sicily Channel, Italy: implications for modelling the magmatic plumbing system." Mineralogical Magazine 66, no. 6 (2002): 953–68. http://dx.doi.org/10.1180/0026461026660070.

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Abstract The Island of Linosa is a small part of the large submarine volcanic complex which is locatedat the SW edge of the Linosa Graben, Sicily Channel. The island was formed between 1.06±0.10 and 0.53±0.07 Ma, through three main stages of activity: Paleo-Linosa, Arena Bianca and Monte Bandiera. Major and trace element data show that the compositional variability of the three activity stages is limited, with most of the rocks showing basaltic to hawaiitic composition. Evolved benmoreites and trachytes are foundas lithics in some pyroclastic units of Paleolinosa. The mafic rocks of the three
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Rivett, Michael O., Shona Symon, Lucas Jacobs, et al. "Paleo-Geohydrology of Lake Chilwa, Malawi is the Source of Localised Groundwater Salinity and Rural Water Supply Challenges." Applied Sciences 10, no. 19 (2020): 6909. http://dx.doi.org/10.3390/app10196909.

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Meeting long-term rural community water supply needs requires diligent geohydrological conceptualisation. Study of Malawi’s Lake Chilwa Basin, including sampling of 330 water points in Phalombe District, enabled assessment of groundwater quality influence upon supply. The control of larger Lake Chilwa paleo-environments on current Basin groundwater quality is demonstrated. Lacustrine sediment deposition forming high-level deposits under open lake conditions and terrace deposits under open and closed lake conditions significantly control the groundwater major-ion quality and salinity now observ
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Wills, W. H., David W. Love, Susan J. Smith, et al. "Water Management at Pueblo Bonito: Evidence from the National Geographic Society Trenches." American Antiquity 81, no. 3 (2016): 449–70. http://dx.doi.org/10.1017/s0002731600003942.

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Recent archaeological investigations at Pueblo Bonito in Chaco Canyon reveal that residents constructed a large diversion channel during the eleventh century A.D. as dramatic growth resulted in the expansion of the building onto the main valley floor. Sediments in the diversion channel reflect repeated episodes of flooding, rather than slow moving water typically found in irrigation canals, and archaeobotanical data indicate deposition during late summer or early fall. Although an agricultural function is possible, the channel may have been built primarily to divert floodwaters away from Puebl
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Château, Chloé C. F., Shahin E. Dashtgard, and James A. MacEachern. "Refinement of the stratigraphic framework for the Regional C depositional unit of the McMurray Formation and implications for the early transgression of the Alberta Foreland Basin, Canada." Journal of Sedimentary Research 90, no. 10 (2020): 1322–45. http://dx.doi.org/10.2110/jsr.2020.62.

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ABSTRACT The Lower Cretaceous McMurray Formation in Alberta and Saskatchewan, Canada, comprises a series of depositional units (DUs) consisting of stacked parasequences bounded by flooding surfaces and incised by fluvio-estuarine channel belts. The fluvio-estuarine channel belts of the McMurray Fm have been the focus of numerous studies whereas the regional DUs have received substantially less attention. Of the regional DUs, Regional C (equivalent to the middle McMurray) is the most understudied, yet this interval records the history of the McMurray Formation between deposition of fluvial stra
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Dissertations / Theses on the topic "Paleo Channel system"

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Walakulu, Arachchige Dilini Madhushani. "Defining Morrow Sandstone Channel System in Manassas Field, Denver Basin, Colorado, USA." OpenSIUC, 2021. https://opensiuc.lib.siu.edu/theses/2879.

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The Manassas oil field was discovered in 1986 in Lincoln County, Colorado (Township 14S, Range 56W) by Petro Lewis Corporation and it completed production from the Pennsylvanian Atoka Sandstone within 24 years. It is located on the theoretical NW extension of the Haswell-Salt Lake Morrow sandstone producing trend and Morrow sandstones have found in some of the available wells in the area. The productive Morrow sandstones are fluvial channel deposits that are encased by marine shales. The distribution of the Morrow channel system is difficult to define from either data obtained from sparsely lo
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Books on the topic "Paleo Channel system"

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Claussen, Martin, Anne Dallmeyer, and Jürgen Bader. Theory and Modeling of the African Humid Period and the Green Sahara. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.532.

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There is ample evidence from palaeobotanic and palaeoclimatic reconstructions that during early and mid-Holocene between some 11,700 years (in some regions, a few thousand years earlier) and some 4200 years ago, subtropical North Africa was much more humid and greener than today. This African Humid Period (AHP) was triggered by changes in the orbital forcing, with the climatic precession as the dominant pacemaker. Climate system modeling in the 1990s revealed that orbital forcing alone cannot explain the large changes in the North African summer monsoon and subsequent ecosystem changes in the
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Jacobsen, Dean, and Olivier Dangles. The high altitude environment. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0001.

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Chapter 1 gives a brief overview of the climatic and terrestrial environment in which high altitude waters are embedded. This context is necessary to understand the prevailing environmental conditions in the aquatic systems. The chapter begins by defining high altitude, alpine, and mountain, and provides an overview of the distribution of the world’s main high altitude regions. The overall picture of the climatic setting is drawn, from the inevitable consequences of high altitude (low temperature, low atmospheric pressure, and high solar radiation) to the highly region-specific patterns in pre
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Book chapters on the topic "Paleo Channel system"

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Kafri, Uri, and Yoseph Yechieli. "Paleo, Current and Future Marine Base-Levels." In Groundwater Base Level Changes and Adjoining Hydrological Systems. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-13944-4_7.

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Fosberg, Michael A., and Samuel Levis. "Reconstruction Of Paleo-Fire Through Climate And Eco-System Models." In Sediment Records of Biomass Burning and Global Change. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-59171-6_4.

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Hahn, Annette, Enno Schefuß, Nicole Burdanowitz, et al. "Catchment and Depositional Studies for the Reconstruction of Past Environmental Change in Southern Africa." In Sustainability of Southern African Ecosystems under Global Change. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_28.

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AbstractTerrestrial signals in marine sedimentary archives are often used for reconstructing past environments, vegetation and climate, as well as for determining sediment fluxes, pathways, and depositional sites and changes in erosional runoff. It is therefore important to understand the origin, transport, and depositional processes of the various terrestrial sedimentary components in a depositional system. In this chapter, we use examples from southern Africa to show how source-to-sink studies have led to a clearer interpretation of downcore proxy records. Twelve rivers in four river catchment areas of various scales and in distinct climatic settings and geological formations are included in this compilation. We also discuss studies from the current-swept South African east coast, the broad western and southern margins, and investigations from protected marine embayment settings. We consider a large suite of commonly used proxies (plant wax isotopes, elemental composition, and fossil pollen) as well as hydroacoustic surveying techniques (PARASOUND and multibeam bathymetric profiling). Sampling strategies and sample types that may be used in catchment analyses are discussed. Challenges and limitations of the above-mentioned approaches are outlined. In conclusion, we underline the importance of a thorough source-to-sink approach to paleo-environmental reconstructions using terrigenous proxies.
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Billy, Julie, Vivien Baudouin, Manuel Garcin, and Gildas Noury. "Beneath the Vendée dunes: former coastal systems, interface between marsh and foreshore revealed by ground-penetrating radar and core-penetration testing." In ASF Publications. Association des Sédimentologistes Français, 2025. https://doi.org/10.70665/ijuh4247.

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The combined use of ground-penetrating radar and geotechnical testing by CPT in Pays-de-Monts (Vendée, France) effectively characterizes the coastal geosystem. The results reveal the internal structure and soil behavior type of coastal dunes and their underlying sedimentary units, highlighting distinct features beneath the dune system at two neighboring sites. At La Parée Grollier, the dunes migrated above former foreshore and marsh deposits, and the study reveals the sub-surface foreshore-marsh transition. At La Pège, a clay-rich paleo-channel was identified which seems connected to the modern beach/dune system. These findings emphasize the value of subsurface data for effective coastal management considering their specific features.
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Craig, R. G. "The Kinematics Of Paleo Landforms." In Computers in Geology - 25 Years of Progress. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195085938.003.0028.

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Reconstructions of past, climates and other applications of global models require specification of landforms arid geomorphic systems as boundary conditions. As general circulation models become more sophisticated and comprehensive and the range of applications for reconstructions grows, there will be an increasing demand for valid geomorphic boundary conditions throughout the Phanerozoic. Geomorphologists have not yet, developed the tools and expertise needed to produce reconstructions, so a major gap in understanding of global change now exists. A strategy to fill that gap is presented here. If geomorphology is the study of the form of the land, and if the form of the land can be described by a set of numbers (digital elevation models), then whither geomorphology? Do we become numericists, mathematicians, and statisticians? If geomorphology is the study of the processes shaping the land, and if the form is completely explained by a set of processes and an initial condition (i.e., landform at some earlier time), then two "knowns," current form and current processes, are essential. But if processes themselves change through time and there is an infinite set, of initial conditions, one set for each point in time, then the job becomes overwhelmingly complex. As the geomorphic community has become painfully aware of the difficulties of deep reconstructions, we have withdrawn into the Quaternary, a period during which many simplifying assumptions can be made which allow solution of geomorphic problems. Hence the Geological Society of America lumps "Quaternary Geology" and "Geomorphology" into one division. We have become so comfortable with the notion that, geomorphology and Quaternary geology are synonymous that we have lost sight of the goals of founders of the science such as William Morris Davis and John Wesley Powell who strove to unearth the landforms of the distant past. Of course there is plenty to keep us busy in the good ol’ Quaternary; but we shouldn't ignore the enormous challenges and opportunities that await those who would reconstruct landforms of earlier times.
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Khiterer, Victoria. "How Jews Gained Their Education in Kiev, 1860–1917." In Polin: Studies in Polish Jewry Volume 30. Liverpool University Press, 2018. http://dx.doi.org/10.3828/liverpool/9781906764500.003.0008.

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RUSSIAN governmental policies on Jewish education changed several times during the nineteenth and early twentieth centuries. As Michael Stanislawski has shown, the Russian government actively intervened in affairs related to the traditional Jewish educational system. The law of 1844 led to the establishment of Jewish state schools in many cities and towns in the Pale of Settlement, subordinating traditional religious Jewish schools, ...
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Bhattacharya, Janok P., and Robert S. Tye. "Searching for Modern Ferron Analogs and Application to Subsurface Interpretation." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c2.

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Abstract A quantitative approach to selecting modern-depositional settings analogous to those of the Cretaceous Ferron Sandstone is presented as well as an approach to using these analogs to improve subsurface interpretations. Paleotectonic, paleogeographic, and climatic setting of the U.S. Western Interior are integrated to estimate the size of the Ferron drainage network to be 50,000 km 2(19,000 mi 2). Estimates of flow depths, flow velocities, and channel cross-sectional areas suggest maximum trunk river paleo-discharge was on the order of 50 × 10 9m 3/year (250 × 10 9ft 3/year). Analogous modern examples include moderate-sized rivers that drain active mountain belts like the Po (Italy), Rhône, (France), and Ebro (Spain). Continental-scale systems, such as the Mississippi (U.S.A.), Niger (West Africa), Amazon (South America), and Nile (North Africa) deltas, are not appropriate analogs. Incised-valley systems within the Ferron are comparable in depth (about 30 m [100 ft]) to distributary channels in more continental-scale systems. A key difference is that Ferron valleys are filled with multiple channel deposits, with individual channel fills less than about 9 m (30 ft) deep. The relatively uniform size of distributary channels suggests that Ferron rivers experienced only a few orders of bifurcation as they flowed across the delta plain. Shoreline and delta-front deposits are wave-influenced. Locally, the basal Ferron deltas were fluvial dominated, although these fluvial-dominated lobes may lie on the downdrift side of asymmetric wave-influenced deltas, similar in plan to the Brazos, Ebro, and Rhône deltas, and to the southern St. George lobe of the Danube delta. Sizes and geometries of various depositional bodies in modern deltas better constrain estimates of inter-well heterogeneity in subsurface correlations. Correlations of Ferron core and wireline-log datasets are compared with the more complete stratigraphy documented in outcrop. Although the broad clinoform geometry of strata in these deposits can be recreated from subsurface correlations, specific parasequences could not be reliably correlated using only the subsurface data. The subsurface-to-outcrop comparison demonstrates a risk of over-correlating reservoir compartments (i.e. non-connected bodies) separated by minor flooding shales within complex, offlapping fluvial-deltaic reservoir deposits. The Ferron outcrop data provides a measure of uncertainties in correlation of subsurface analogs.
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Bianchi, Thomas S., and Elizabeth A. Canuel. "Chemical Biomarker Applications to Ecology and Paleoecology." In Chemical Biomarkers in Aquatic Ecosystems. Princeton University Press, 2011. http://dx.doi.org/10.23943/princeton/9780691134147.003.0002.

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This chapter provides a brief historical account of the success and limitations of using chemical biomarkers in aquatic ecosystems. It also introduces the general concepts of chemical biomarkers as they relate to global biogeochemical cycling. The application of chemical biomarkers in modern and/or ancient ecosystems is largely a function of the inherent structure and stability of the molecule, as well as the physicochemical environment of the system wherein it exists. In some cases, redox changes in sediments have allowed for greater preservation of biomarker compounds; in well-defined laminated sediments; for example, a strong case can be made for paleo-reconstruction of past organic matter composition sources. However, many of the labile chemical biomarkers may be lost or transformed within minutes to hours of being released from the cell from processes such as bacterial and/or metazoan grazing, cell lysis, and photochemical breakdown. The role of trophic effects versus large-scale physiochemical gradients in preserving or destroying the integrity of chemical biomarkers varies greatly across different ecosystems. These effects are discussed as they relate to aquatic systems such as lakes, estuaries, and oceans.
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Dabbagh, Abdallah E., Khattab G. Al-Hinai, and M. AsiF Khan. "Evaluation of the Shuttle Imaging Radar (SIR-C/X-SAR) data for mapping paleo-drainage systems in the Kingdom of Saudi Arabia." In Quaternary Deserts and Climatic Change. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077862-49.

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Mayes, Maureen D. "Raynaud’s Phenomenon, Skin Involvement, and Finger Sores." In The Scleroderma Book. Oxford University PressNew York, NY, 1999. http://dx.doi.org/10.1093/oso/9780195115079.003.0007.

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Abstract This chapter relates to people with the systemic form of scleroderma, including both those with limited disease and those with diffuse disease. It does not apply to people with localized scleroderma, which is morphea and linear scleroderma. Raynaud’s phenomenon Raynaud’s phenomenon is a specific type of cold sensitivity that is characterized by color changes of the fingertips on cold exposure. There is some variation from one person to the next, but the typical Raynaud’s episode starts with the fingertips getting very pale, then numb, and then turning a purple or blue color.
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Conference papers on the topic "Paleo Channel system"

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Ellen, H., Abdulla AlAli, A. T. Ajayi, and H. Guney. "Applied Sequence Stratigraphy Combined with Geological Modeling of the Greater Cheleken Area (Central Caspian Basin, Turkmenistan) Using New 3D OBN Acquisition to Reveal Channel Complex Systems from Delta to Deepwater Environments in Plio-Pleistocene Clastic Reservoirs." In ADIPEC. SPE, 2024. http://dx.doi.org/10.2118/222672-ms.

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Abstract The Greater Cheleken Area (GCA) reservoirs, developed offshore by Dragon Oil, are located along a complex NW-SE dextral transcurrent zone that separates the Northern and Southern Caspian Basins (SCB). This area hosts numerous hydrocarbon fields within thick, highly faulted Pliocene-Pleistocene clastic successions of the paleo-Amu-Darya Delta System, originating in the N-Balkan Fold Belt. We present a new model for the geological evolution of this region, based on the analysis and sequence stratigraphy interpretation of new 3D OBN seismic data, well logs, and integration with existing
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Pandolpho, Bruna, Gilmar Bueno, Arthur Machado, Carlos Theodoro, Antonio Fernando Filho, and Antonio Henrique Klein. "Morphology of submarine channels and paleo-flow discharge estimation_ Itabapoana turbidity system, Campos Basin." In International Congress of the Brazilian Geophysical Society&Expogef. Brazilian Geophysical Society, 2019. http://dx.doi.org/10.22564/16cisbgf2019.132.

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Monacchi, David. "The sonic heritage of ecosystems." In SOIMA 2015: Unlocking Sound and Image Heritage. International Centre for the Study of the Preservation and Restoration of Cultural Property, 2017. http://dx.doi.org/10.18146/soima2015.3.12.

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This paper discusses the importance of the ‘paleo- soundscapes’ of remote natural habitats as unique footprints of the systemic behaviour of healthy ecosystems and proposes considering them as intangible heritage to be urgently recorded and preserved. The interdisciplinary project Fragments of Extinction has worked toward preserving that ecological heritage through multidimensional sound recording eldwork in primary equatorial rainforests since 2002. The soundscapes of these unique, untouched and undisturbed places – increasingly threatened by human pressure and climate change – represent an o
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Benny, Hendra, Teekayu Benjawan, Kasame Chaichana, et al. "Play-Based Evaluation on Permian Carbonate Reservoir: Implications for Petroleum Exploration in Northeast Thailand." In International Petroleum Technology Conference. IPTC, 2023. http://dx.doi.org/10.2523/iptc-22828-ea.

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Abstract Despite the long exploration history, success rate has been low in the Khorat Plateau region of northeastern Thailand. To date, only two gas fields (from 9 discoveries) have been produced from Permian carbonate reservoirs, the only successful play. PTTEP and Department of Mineral Fuels (DMF) of Thailand conducted a collaborative basin-wide study using a Play-Based Exploration (PBE) method to fully understand the remaining prospectivity. PBE combines all aspects of petroleum system to provide a holistic view on basin prospectivity. It integrates existing knowledge in literature with we
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Zamanbayov, Ulvi. "Seismic Facies Analysis of Lower Productive Series of Gurgan-Deniz Field in South Caspian Basin with the Aid of Seismic Attributes." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207047-ms.

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Abstract Drilled for the first time in 1946 and one of the oldest fields in the South Caspian Basin located in the western part of Apsheron sill, Gurgan-Deniz has been subject to redevelopment. A 3D seismic survey, conducted over the area for the first time, has been interpreted, analysing the lower Productive Series with regard to seismic facies and prospectivity. The facies analysis allows for better understanding of eustatic levels in the region and depositional environments of lower Productive Series in the area. A composite seismic attribute Sweetness and an RGB blend of Spectral Decompos
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Zamanbayov, Ulvi. "Seismic Facies Analysis of Lower Productive Series of Gurgan-Deniz Field in South Caspian Basin with the Aid of Seismic Attributes." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207047-ms.

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Abstract Drilled for the first time in 1946 and one of the oldest fields in the South Caspian Basin located in the western part of Apsheron sill, Gurgan-Deniz has been subject to redevelopment. A 3D seismic survey, conducted over the area for the first time, has been interpreted, analysing the lower Productive Series with regard to seismic facies and prospectivity. The facies analysis allows for better understanding of eustatic levels in the region and depositional environments of lower Productive Series in the area. A composite seismic attribute Sweetness and an RGB blend of Spectral Decompos
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Kusdiantoro, F. "The Arang Petroleum Play in The West Natuna Basin: A New Perspective From Geochemical Study and Petroleum System Modelling." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-g-67.

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One of the main producing gas reservoirs in the Medco E&P Natuna Ltd.’s (Medco E&P) operated South Natuna Sea Block B PSC (Block B) is the shallow Miocene Arang Formation (Arang reservoir or Arang). The main characteristics of the Arang gas is the dominance of the dry component. The previous understanding was that the gas was generated from the Arang intra-formational shale source rock. An integrated geochemical and regional 3D petroleum system model has been conducted over the Block B area. This effort suggests that the main contributing source rock to the Arang reservoir is in fact t
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Masud, Luciana, Verónica Lorena Cortez, Mario Antonio Ottulich, et al. "Gas Lift Optimization in Unconventional Wells – Vaca Muerta Case Study." In SPE Argentina Exploration and Production of Unconventional Resources Symposium. SPE, 2023. http://dx.doi.org/10.2118/212577-ms.

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Abstract Gas lift was the selected artificial lift system for Vaca Muerta formation in the Bajada del Palo Oeste field, a shale oil reservoir in Argentina. At an early stage, the main goal was to successfully overcome the design challenge of facilities and downhole installation for wells with very wide and constantly changing liquid production ranges. At a later stage, to establish an optimization methodology that could be updated at a rate comparable to production changes. Several projects were implemented for optimizing the gas lift field. First, work was oriented toward improving the preven
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Reports on the topic "Paleo Channel system"

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Ziesler, Pamela, and Claire Spalding. Statistical abstract: 2021. National Park Service, 2022. http://dx.doi.org/10.36967/nrds-2293345.

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Abstract:
In 2021, recreation visits to National Park Service (NPS) sites rebounded from the COVID-19 pandemic-driven low visitation of 2020 and climbed to 297,115,406 recreation visits. This is an increase of 60 million recreation visits (+25.3%) from 2020 and a decrease of 30 million recreation visits (-9.3%) from 2019. Recreation visitor hours were 1,356,657,749 – a 28.6% increase from 2020 and a 5.1% decrease from 2019. Total overnight stays followed a similar pattern with 12,745,455 overnight stays – up 4.7 million (+58.5%) from 2020 and down 1.1 million (-8%) from 2019. Five parks were added to th
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