Relevant bibliographies by topics / Facies of siliceous porifera

Contents

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

Academic literature on the topic 'Facies of siliceous porifera'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Facies of siliceous porifera.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Facies of siliceous porifera"

1

Hostettler, Bernhard, and Ursula. Menkveld-Gfeller. "Die Cidariden (Echinoidea, Echinodermata) der Wildegg-Formation (mittleres Oxfordien, Schweizer Jura)." Revue de Paléobiologie 34, no. 2 (2015): 195–233. https://doi.org/10.5281/zenodo.34342.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Bavestrello, Giorgio, Attilio Arillo, Barbara Calcinai, et al. "Siliceous particles incorporation inChondrosia reniformis(Porifera, demospongiae)." Italian Journal of Zoology 65, no. 4 (1998): 343–48. http://dx.doi.org/10.1080/11250009809386771.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Du, Yushan, Na Yin, Qinhong Hu, et al. "Quantitative Characterization of Full-Spectrum Pore Size and Connectivity for Shale with Different Sedimentary Facies from the Dongying Depression, Bohai Bay Basin, East China." Geofluids 2022 (May 31, 2022): 1–17. http://dx.doi.org/10.1155/2022/9744086.

Full text
Abstract:
Working with shales in the fourth member of Shahejie Formation in the Dongying Depression in Bohai Bay Basin of East China, this study examines the facies classification, petrological characteristics, pore size distribution, and pore connectivity of oil-producing shale. The studied shales could be classified into five sedimentary facies according to a three-step classification criterion that consists of total organic carbon (TOC), sedimentary structure, and mineral composition. Among them, the “low TOC massive siliceous mudstone” and “low TOC layered clayey mudstone” facies have similar distri
APA, Harvard, Vancouver, ISO, and other styles
4

Stasiuk, L. D., and M. G. Fowler. "Organic facies in Devonian and Mississippian strata of Western Canada Sedimentary Basin: relation to kerogen type, paleoenvironment, and paleogeography." Bulletin of Canadian Petroleum Geology 52, no. 3 (2004): 234–55. http://dx.doi.org/10.2113/52.3.234.

Full text
Abstract:
Abstract Petrographic analyses of dispersed organic matter (including macerals and palynomorphs), siliceous and calcareous microfossil assemblages and microtextures (e.g. stromatolitic) have been used to define and interpret five organic facies and regionally map their distribution for the following informal groupings of potential hydrocarbon source rocks in the Western Canada Sedimentary Basin: Upper Devonian Woodbend group, Upper Devonian Winterburn group and Upper Devonian to Lower Mississippian black shales of the Exshaw and Bakken formations. Five petrographic organic facies (A–E) are def
APA, Harvard, Vancouver, ISO, and other styles
5

Soua, Mohamed. "Application of Facies Associations, Integrated Prediction Error Filter Analysis, and Chemostratigraphy to the Organic-Rich and Siliceous Cenomanian-Turonian Sequence, Bargou Area, Tunisia: Integrated Sequence Stratigraphic Analysis." Journal of Geological Research 2012 (June 13, 2012): 1–15. http://dx.doi.org/10.1155/2012/973195.

Full text
Abstract:
Facies associations, integrated prediction error filter analysis (INPEFA) of spectral Gamma-ray data, Sr/Ca and Mn chemostratigraphy, and sequence stratigraphy of the organic-rich and siliceous Cenomanian-Turonian Bahloul formation have been studied in Bargou section, located in north-central Tunisia. The studied section is subdivided into seven facies evolving from platform to basin deposits. Based on basin geometry, facies distribution, spectral Gamma-ray INPEFA curves, Sr/Ca and Mn profiles patterns, and the sequence was also subdivided into shelf margin wedge (uppermost Fahden Formation-lo
APA, Harvard, Vancouver, ISO, and other styles
6

Domack, Eugene W., and P. T. Harris. "A new depositional model for ice shelves, based upon sediment cores from the Ross Sea and the MaC. Robertson shelf, Antarctica." Annals of Glaciology 27 (1998): 281–84. http://dx.doi.org/10.3189/1998aog27-1-281-284.

Full text
Abstract:
We document the similarity of depositional facies occurring in gravity cores recovered from two disjunct regions of the Antarctic continental shelf: the Ross Sea and the MaC. Robertson shelf. The facies sequence model is represented in two cores, one collected during the 1995-1 cruise of the R/VNathaniel R. Palmer(core NBP95 TC-18) and the other collected by the RSVAurora Australisduring cruise 149 in 1995 (core 149 39GC38). Both cores show a succession of facies indicative of ice-shelf retreat during the late-Pleistocene to Holocene transition. Distinct lithofacies range in thickness from a f
APA, Harvard, Vancouver, ISO, and other styles
7

Guidry, Sean A., and Henry S. Chafetz. "Siliceous shrubs in hot springs from Yellowstone National Park, Wyoming, U.S.A." Canadian Journal of Earth Sciences 40, no. 11 (2003): 1571–83. http://dx.doi.org/10.1139/e03-069.

Full text
Abstract:
Many of the siliceous hot springs in Yellowstone National Park contain subaqueous, spinose siliceous precipitates up to 5 cm high that occupy shallow terracettes in siliceous terraced mound accumulations, discharge channels, etc. These siliceous "shrubs" are composed of opal-A with an arborescent or branching pattern and have strong morphological similarities to bacterial shrubs from carbonate-precipitating hot springs. Siliceous shrubs constitute a major precipitate style associated with discharge channel – flow-path facies throughout most of the 20 m of flow path at Cistern Spring, Norris Ge
APA, Harvard, Vancouver, ISO, and other styles
8

Artushkova, O. V., and V. A. Maslov. "Devonian succession in the East-Zilair zone: conodont-based subdivision and paleontological verification." LITHOSPHERE (Russia) 22, no. 1 (2022): 14–38. http://dx.doi.org/10.24930/1681-9004-2022-22-1-14-38.

Full text
Abstract:
Research subject. Conodont-based biostratigraphic subdivision of the monotonous siliceous-terrigenous sequence stratigraphically underlying the Famennian Zilair Formation.Materials and methods. Conodont imprints on the bedding planes from our own collections along with the data from other researchers were used for dating and subdivision of siliceous formations.Results. Our study of conodonts from the deposits underlying the Zilair Formation at a number of intersections on the eastern side of the Zilair synclinorium showed that the stratigraphic scale of the straton, previously recognised as th
APA, Harvard, Vancouver, ISO, and other styles
9

Jati Widiatama, Angga, Achmad Fahruddin, and Lauti Dwita Santy. "Characteristics of polymetallic enrichment on oceanic red bed in Matano Formation, Baturubei, Central Sulawesi, Indonesia." IOP Conference Series: Earth and Environmental Science 882, no. 1 (2021): 012045. http://dx.doi.org/10.1088/1755-1315/882/1/012045.

Full text
Abstract:
Abstract The Matano Formation on Sulawesi Island has Cretaceous oceanic red bed (CORB) facies, but there is no further research on the geochemical characteristics of the sedimentary rocks. This study aims to classify the CORB of the Matano Formation and reveal the polymetallic element enrichment in CORB by using the X-ray fluorescence (XRF) analysis method. Matano Formation in the research area consists of two different facies: radiolarites facies and red clay facies. Radiolarites facies grouped as Si-ORB, dominated by siliceous pelagic bioclastic and deposited under oxic environment. The red
APA, Harvard, Vancouver, ISO, and other styles
10

Pervushov, Evgeny M. "Colonial Leptophragmidae (Porifera, Hexactinellida) from the Lower Santonian of the Volga region." Izvestiya of Saratov University. Earth Sciences 23, no. 1 (2023): 53–60. http://dx.doi.org/10.18500/1819-7663-2023-23-1-53-60.

Full text
Abstract:
Study of the skeletal morphology of a new representative of the Leptophragmidae family, with no suboscula in its structure, provides support for the earlierspecified regularities in generation of Hexactinellida modular forms. Good preservationstate of a majorcolony has made it possible to specify the aspects of paleoecology and taphonomy in the later representatives of the Middle Coniacian – Early Santonian succession of siliceous sponges.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Facies of siliceous porifera"

1

Frisone, Viviana. "Eocene siliceous sponges (porifera: hexactinellida, demospongea) from eastern Lessini mountains (northen italy)." Doctoral thesis, Università degli studi di Padova, 2014. http://hdl.handle.net/11577/3423786.

Full text
Abstract:
2 case studies of Eocene siliceous sponges from Eastern Lessini Mountains are reported. Case study 1— Bartonian Mt. Duello isolated spicules (Verona). This study documents exceptionally preserved isolated opaline spicules, unique for the Middle Eocene (Bartonian) of Italy. Interpretation of morphological types of spicules by comparison with living species lead to their attribution to 5 orders (Astrophorida, Hadromerida, Haplosclerida, Poecilosclerida, “Lithistida”), 7 families (Geodiidae, Placospongiidae, Tethyidae, Petrosiidae, Acarnidae, ?Corallistidae, Theonellidae) and 5 genera (Geodia,
APA, Harvard, Vancouver, ISO, and other styles
2

Kastigar, Jessica M. "Application of X-ray Computed Tomography to Interpreting the Origin and Fossil Content of Siliceous Concretions from the Conasauga Formation (Cambrian) of Georgia and Alabama, USA." The Ohio State University, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=osu1461271051.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Book chapters on the topic "Facies of siliceous porifera"

1

Maurrasse, Florentin J.-M. R. "Taxonomy, biostratigraphy, and paleoecologic significance of calcareous-siliceous facies of the Neogene Montpelier Formation, northeastern Jamaica." In Biostratigraphy of Jamaica. Geological Society of America, 1993. http://dx.doi.org/10.1130/mem182-p255.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Potma, K., R. Jonk, and K. M. Bohacs. "10 Canol Formation, Northwest Territories, Canada—An Outcrop-to-Subsurface Analog for the Paleozoic Horn River Shale-gas Play." In Sequence Stratigraphy: Applications to Fine-Grained Rocks. The American Association of Petroleum Geologists and Brazilpetrostudies, 2022. http://dx.doi.org/10.1306/137123053861.

Full text
Abstract:
ABSTRACT The Late Devonian Canol Formation and associated stratal units in the Northwest Territories of Canada illustrate the expression of sequence-stratigraphic surfaces and units in a distal Paleozoic carbonate shelf to relatively deep-basin setting. These Devonian strata are time equivalent and quite analogous in depositional conditions and petroleum-system characteristics to the proven shale-gas deposits in the Horn River Basin of northeastern British Columbia. The Canol Depositional Sequence spans the upper part of the Ramparts Formation, the Canol Formation, and the lowermost part of th
APA, Harvard, Vancouver, ISO, and other styles
3

Blake, Gregg H. "Relationship of organic carbon deposition in the Monterey Formation to the Monterey excursion event based on an updated chronostratigraphic framework of the Naples Beach section, California." In Understanding the Monterey Formation and Similar Biosiliceous Units across Space and Time. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2556(07).

Full text
Abstract:
ABSTRACT The Monterey Formation, consisting of siliceous and calcareous biogenic sediments, was deposited during the transition from a relatively warm greenhouse climate in the early Miocene to the cooler temperatures of icehouse climatic conditions during the early middle to late Miocene. This cooling event was associated with global paleoclimatic and oceanic changes assumed to be related to the deposition of organic carbon–rich sediments into the marginal basins of California. This chapter introduces an age model for the Miocene strata at Naples Beach based on a composite stratigraphic secti
APA, Harvard, Vancouver, ISO, and other styles
4

Soua, Mohamed, Hela Fakhfakh-Ben, Dalila Zaghbib-Turki, et al. "The Organic-Rich and Siliceous Bahloul Formation: Environmental Evolution Using Facies Analysis and Sr/Ca & Mn Chemostratigraphy, Bargou Area, Tunisia." In Earth and Environmental Sciences. InTech, 2011. http://dx.doi.org/10.5772/24391.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Volkert, Richard A. "Geologic Setting of Proterozoic Iron, Zinc, and Graphite Deposits, New Jersey Highlands." In Part I. Proterozoic Iron and Zinc Deposits of the Adirondack Mountains of New York and the New Jersey Highlands Part II. Environmental Geochemistry and Mining History of Massive Sulfide Deposits in the Vermont Copper Belt. Society of Economic Geologists, 2001. http://dx.doi.org/10.5382/gb.35.07.

Full text
Abstract:
Abstract The New Jersey Highlands are underlain principally by Mesoproterozoic rocks that were metamorphosed at upper amphibolite to granulite facies between 1080 and1030 Ma during the Ottowan Orogeny. The oldest rocks are inferred to be metamorphosed ca. 1300 Ma dacite, tonalite, and trondhjemite and associated charnockitic plutonic and metavolcanic rocks of the Losee Metamorphic Suite. These originated in a continental margin magmatic arc setting dominated by calc-alkaline and tholeiitic magmatism. Rocks of the Losee record a compressional event in the north-central Appalachians that was lik
APA, Harvard, Vancouver, ISO, and other styles
6

Bohacs, K. M., and A. Ferrin. "13 Monterey Formation, Miocene, California, U.S.A.—A Cenozoic Biosiliceous-Dominated Continental Slope to Basin Setting: A Billion-Barrel Deep-Water Mudstone Reservoir and Source Rock." In Sequence Stratigraphy: Applications to Fine-Grained Rocks. The American Association of Petroleum Geologists and Brazilpetrostudies, 2022. http://dx.doi.org/10.1306/137123081283.

Full text
Abstract:
ABSTRACT The Monterey Formation illustrates the expression of sequence-stratigraphic surfaces and units in continental slope and basin settings that are quite unlike those of most mudstone units considered thus far in this book. These strata span a wide variety of siliceous, calcareous, argillaceous, phosphatic, and kerogenous composition, detrital, biogenic, and authigenic origins, and clay to cobble grain size. The Monterey Formation poses particular challenges with its deposition of dominantly biogenic sediments in a variety of deep-basinal environs in an active tectonic region. This chapte
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Facies of siliceous porifera"

1

Bellas, S., D. Telemenis, V. Makri, I. Oikonomopoulos, E. Tripsanas, and E. Manoutsoglou. "Enriching the Source Rocks of Greece; Geochemical Evaluation of Neogene Marine Siliceous Facies from Crete Island." In Fourth EAGE Eastern Mediterranean Workshop. European Association of Geoscientists & Engineers, 2023. http://dx.doi.org/10.3997/2214-4609.202330019.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Snachev, А. V., K. R. Nurieva, and R. R. Islamov. "GEOLOGY OF CARBONACEOUS DEPOSITS OF THE BIRGILDA STRATA (EAST URAL TROUGH)." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. Пермский государственный национальный исследовательский университет, 2021. http://dx.doi.org/10.17072/chirvinsky.2021.223.

Full text
Abstract:
The article describes the geological structure of the Birgilda strata, which is widely developed in the East Ural trough. It is shown that the Birgilda black shales, which contain Corg in the range of 0.5–2.7% (average 1.3%), are of the low-carbon type. The exothermic effect in them occurred mainly in the temperature range 570–660 ° С, which corresponds to the greenschist facies of regional metamorphism. On the A-S-C diagram, the rocks of the Birgilda strata are approximately equally scattered over the carbonate-carbonaceous and siliceous-carbonaceous fields and noticeably less in the terrigen
APA, Harvard, Vancouver, ISO, and other styles
3

Abu-Mahfouz, Israa S., Maria Ardila, and Volker Vahrenkamp. "Geochemical and Petrographic Characteristics of Lithofacies from Upper Cretaceous Organic-Rich Source Rocks, Jordan." In International Petroleum Technology Conference. IPTC, 2022. http://dx.doi.org/10.2523/iptc-21914-ms.

Full text
Abstract:
Abstract The Upper Cretaceous source rocks of Jordan are organic-rich carbonate mudrocks that represent excellent source rocks but are essentially still immature to just entering the oil window. Therefore, they offer a unique opportunity to study lithology, source rock composition, and geochemistry prior to the onset of maturation and expulsion of hydrocarbons. Our study aims to examine the lithological and geochemical characteristics of these high-quality source rocks. The study utilizes an integrated petrographic and geochemical approach to define the different microfacies in the studied sou
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Facies of siliceous porifera"

1

Kuster, K., C. M. Lesher, and M. G. Houlé. Geology and geochemistry of mafic and ultramafic bodies in the Shebandowan mine area, Wawa-Abitibi terrane: implications for Ni-Cu-(PGE) and Cr-(PGE) mineralization, Ontario and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329394.

Full text
Abstract:
The Shebandowan Ni-Cu-(PGE) deposit occurs in the Shebandowan greenstone belt in the Wawa-Abitibi terrane. This deposit is one of a few economic Ni-Cu-(PGE) deposits in the Superior Province and one of a very few deposits worldwide that contains both Ni-Cu-(PGE) and Cr-(PGE) mineralization. The mafic-ultramafic successions in the area comprise abundant flows and sills of tholeiitic basalt and lesser Al-undepleted komatiite (MgO >18 wt%, Al2O3/TiO2 = 15-25), the latter indicating separation from mantle sources at shallow levels. Siliceous high-Mg basalts (MgO 8-12 wt%, SiO2 &
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Facies of siliceous porifera' for particular source types:
Journal articles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography