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Relevant bibliographies by topics / Bucegi Conglomerates

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Academic literature on the topic 'Bucegi Conglomerates'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Bucegi Conglomerates"

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JIPA, Dan Constatin, Constantin UNGUREANU, and Gabriel ION. "Stratigraphy and tectonics of the uppermost Bucegi Conglomerate Formation (Albian, Eastern Carpathians, Romania)." Geo-Eco-Marina No 19/2013 (December 31, 2013): 113–27. https://doi.org/10.5281/zenodo.56849.

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Abstract. This paper presents a detailed lithostratigraphic investigation carried out in the Bucegi Massif, a mountainous zone from the southern part of the Eastern Carpathians. The study focused on the 50 - 70 m thick succession of four conglomerate units associated with olistoliths, intercalated in the upper part of the Babele Sandstone Member (the uppermost lithostratigraphic unit of the Albian Bucegi Conglomerate Formation). The conglomerate beds succession stands for the uppermost strata of the thick Bucegi conglomeratic accumulation. All the four conglomerate bodies are stratiform and co

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Jipa, Dan C., and Cornel Olariu. "Significance of the Bucegi Conglomerate olistoliths in the Albian source-to-sink system from the Carpathian Bend basin in Romania." Interpretation 6, no. 1 (2018): T29—T37. http://dx.doi.org/10.1190/int-2017-0030.1.

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The presence of exotic blocks (or olistoliths) in sedimentary deposits is usually regarded as an indication of a deepwater slope environment. We evaluate olistoliths accumulated in shallow water at the upper edge of a slope setting using outcrop data. The study area is in the Bucegi Mountains in the southeast “bend” of the Carpathian Mountains in Romania. The studied deposits belong to the Bucegi Formation, a dominantly conglomerate succession of Albian age. The Lower Bucegi member has been accumulated as a large conglomerate submarine fan. The Upper Member forms a shelf-to-trench sedimentary

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BRICEAG, Andrei, Dan JIPA, and Mihaela Carmen MELINTE. "Early Cretaceous Deposits of the Ceahlău Nappe (Romanian Carpathian Bend Region)." Geo-Eco-Marina No 15/2009 (December 31, 2009): 37–45. https://doi.org/10.5281/zenodo.57309.

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Abstract. The investigations carried out in the bend area of the Romanian Carpathians (the Bucegi Mts.) indicate that a continuous sedimentation took place within the Early Cretaceous (interval covered by the NJK-NJK3 and NC4-NC8 Calcareous Nannoplankton Zones). The base of the Bucegi Conglomerates is placed within the earliest Albian (in the NC8 Calcareous Nannoplankton Zone). The detailed sedimentological studies focussed on the Bucegi Conglomerates indicate that the sediments are of orthoconglomerate type, containing mainly sub-rounded clasts, which prevailed over the matrix.

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Panin, N. "IN MEMORIAM Dan Constantin Jipa (1935-2020)." Geo-ECo-Marina 26 (2020) (December 31, 2020): 211–18. https://doi.org/10.5281/zenodo.4700306.

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Dan Constantin Jipa, a great friend, an eminent, brilliant scientist, who has completely dedicated his life to Earth Sciences, passed away on September 28, 2020. Adieu dear friend! He worked with total dedication for over 60 years and his enthusiasm and interest in the profession did not fade even at the last moment - two months earlier, he was in the Bucegi Mountains where he had resumed his study of the Bucegi Conglomerates. We were good friends, we worked together and we supported each other to the best of our ability.

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JIPA, Dan C., Cornel OLARIU, and Andrei BRICEAG. "Patrulius Olistolith – A large jurassic limestone block in Albian Conglomerates of the Bucegi Mountains, Southeast Carpathians, Romania." Geo-Eco-Marina No 24/2018 (December 31, 2018): 69–80. https://doi.org/10.5281/zenodo.2549578.

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The paper introduces and describes the Patrulius Olistolith, one of the largest exotic blocks (218 m long, 110 m wide and 55 m thick) embedded in Albian conglomerates from the Carpathian Bend area (southern part of Eastern Carpathians, Romania). The Albian conglomerates embedding the Patrulius Olistolith are deposits with homogeneous internal structure and poor sorting, features typical of debris flow sediments. Based on this character, it is considered that the Patrulius Olistolith transport was a gravitational collapse process and that it was transported as a very large c

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JIPA, C. Dan. "An isolated olistolith in the Ciucaş Conglomerates (Albian, Carpathian Bend)." Geo-Eco-Marina No 22/2016, no. 7 (2016): 135–44. https://doi.org/10.5281/zenodo.889904.

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In the eastern part of the Ciucaș Mountains (Carpathian Bend area) an 18 m long limestone block was located. Unlike the numerous Albian Bucegi olistoliths included in shallow-waters shelf sediments, this is the first olistolith identified in the Albian deep sea fan sediments from the Carpathian Bend area. Structureless rudites are embedding the Ciucaș olistolith, suggesting that rudites and olistolith were transported together due to sediment gravity flow processes. Two Ciucaș olistolith provenance hypotheses are discussed including a local or a distal source area.

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JIPA, D.C., M. MELINTE-DOBRINESCU, and M.A. RUTKA. "LARGE-SCALE PROGRADATION AND SEDIMENT GRAVITY FLOW IN A DEEP-SEA BASIN: ALBIAN DEPOSITS IN THE SOUTH CARPATHIANS (IALOMIȚA-DÂMBOVIȚA AREA, ROMANIA)." Geo-Eco-Marina 26 (2020) (December 31, 2020): 67–99. https://doi.org/10.5281/zenodo.4683112.

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Abstract. This paper summarizes the results of a sedimentologic investigation of Albian sandstones and conglomerates from the eastern extremity of the Southern Carpathians, the area between the Ialomița and Dâmbovița rivers. Lithofacies analysis, paleotransport, provenance and paleoenvironment of these clastic sediments are the main focus of the paper. An important component of the study is the part played by Ialomița-Dâmbovița Albian sediment accumulation in the Albian sedimentary history of the Carpathian Bend zone. Two major lithofacies occur in the Ialomița-Dâmbovița Albi

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Eguiluz y de Antuñano, Samuel. "Contribución al conocimiento geológico del Mesozoico en la parte Norte del Terreno Tahué, México." Boletín de la Sociedad Geológica Mexicana 77, no. 1 (2025): A041124. https://doi.org/10.18268/bsgm2025v77n1a041124.

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La estratigrafía de las unidades vulcano- sedimentarias, marinas y continentales del Mesozoico en la Sierra Madre Occidental ha sido poco documentada, debido a que la mayoría de los estudios se centran en la cubierta volcánica más joven del Oligoceno-Neógeno. Este trabajo aporta datos nuevos sobre la litología, los ambientes de depósito y la cronología de las unidades que afloran en un área de aproximadamente 30,000 km² en las barrancas de Durango y Sinaloa, al norte del Terreno Tahué. Se reconocen tres secuencias estratigráficas separadas por discordancias mayores. La secuencia I, asignada a

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ANASTASIU, Nicolae, Mihai CIOCÂRDEL, and Dan C. JIPA. "NATURE AND PROVENANCE OF THE BUCEGI CONGLOMERATE PEBBLES. A PETROGRAPHIC APPROACH." January 1, 2016. https://doi.org/10.5281/zenodo.45067.

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<strong>Abstract.</strong> This study deals with the provenance and identification of the pebbles belonging to the Bucegi Conglomerates (Albian, Carpathian Bend area). More than 150 thin sections were examined, the samples including magmatic, metamorphic and sedimentary pebbles sampled from 12 occurrences located in the Bucegi Mountains. The classification schemes recommended by IUGS were used for the petrographic identification of the magmatic, metamorphic, and sedimentary clasts. The frequency of the major petrotypes is the following: 70% sedimentary lithoclasts; 10% plutonic lithoclasts; 2%

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Conference papers on the topic "Bucegi Conglomerates"

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Ciocirdel, Mihai. "THE RIETVELD STRUCTURE REFINEMENT OF THE EPIDOTE CRYSTALS FROM BUCEGI CONGLOMERATES (ROMANIA) USING X-RAY POWDER DIFFRACTION DATA." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s01.029.

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