Relevant bibliographies by topics / Neogen

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Academic literature on the topic 'Neogen'

Author: Grafiati
Published: 4 June 2021
Last updated: 16 June 2025

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Journal articles on the topic "Neogen"

1

An Nahar, Rikza Nur Faqih, Angga Jati Widiatama, Lauti Dwita Santy, et al. "Biostratigrafi Nanofosil Gampingan dan Lingkungan Pengendapan Formasi Ofu selama Neogen." Journal of Science and Applicative Technology 5, no. 2 (2021): 348. http://dx.doi.org/10.35472/jsat.v5i2.383.

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Formasi Ofu berumur Neogen-Kuarter tersingkap baik di bagian tengah Pulau Timor. Kumpulan nannofosil gampingan Formasi Ofu berumur Neogen terdiri tujuh famili dan 25 spesies. Nannofosil gampingan berumur Neogen didominasi genus Discoaster, Dictyococcites, dan Reticulofenestra sedangkan umur Kuarter didominasi oleh genus Gephyrocapsa. Nannofosil gampingan Neogen terdiri dari dua zonasi, dan satu zona Kuarter. Permulaan Miosen, Burdigalian-Tortonian (zona NN 4-NN 10) ditandai pemunculan awal Reticulofenestra pseudoumbilica hingga pemunculan awal Discoaster quinqueramus. Zona NN11 yang berumur Tortonian-Messinian ditandai pemunculan awal hingga pemunculan akhir Discoaster quinqueramus. Kuarter (Zona NN20) ditandai pemunculan awal Ponthospaera indooceanica.
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Dorantes-Aranda, Juan José, Aiko Hayashi, Alison R. Turnbull, Jessica Y. C. Jolley, D. Tim Harwood, and Gustaaf M. Hallegraeff. "Detection of Paralytic Shellfish Toxins in Southern Rock Lobster Jasus edwardsii Using the Qualitative Neogen™ Lateral Flow Immunoassay: Single-Laboratory Validation." Journal of AOAC INTERNATIONAL 103, no. 3 (2020): 784–91. http://dx.doi.org/10.1093/jaocint/qsz029.

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Abstract Background Paralytic shellfish toxins (PST) are a significant problem for the Tasmanian shellfish and Southern Rock Lobster (Jasus edwardsii) industries, and the introduction of a rapid screening test in the monitoring program could save time and money. Objective The aim was to perform a single-laboratory validation of the Neogen rapid test for PST in the hepatopancreas of Southern Rock Lobster. Methods The AOAC INTERNATIONAL guidelines for the validation of qualitative binary chemistry methods were followed. Three different PST profiles (mixtures) were used, of which two were commonly found in naturally contaminated lobster hepatopancreas (high in gonyautoxin 2&3 and saxitoxin), and the third toxin profile was observed in a few select animals (high in gonyautoxin 1&4). Results The Neogen test consistently returned negative results for non-target toxins (selectivity). The probability of detection (POD) of PST in the lobster hepatopancreas using the Neogen test increased with increasing PST concentrations. POD values of 1.0 were obtained at ≥0.57 mg STX-diHCl eq/kg in mixtures 1 and 2, and 0.95 and 1.0 for mixture 3 at 0.79 and 1.21 mg STX-diHCl eq/kg, respectively, with a fitted POD of 0.98 for 0.80 mg STX-diHCl eq/kg. The performance of the Neogen test when using four different production lots (ruggedness) showed no significant differences. Conclusions The results of the validation study were satisfactory and the Neogen test is being trialed within the Tasmanian PST monitoring program of Southern Rock Lobster. Highlights The Neogen rapid kit was successfully validated for the detection of PST in Southern Rock Lobster hepatopancreas.
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Ricardo, Nomensen, Hendra Amijaya, and Salahuddin Husein. "Basin Evolution Palispatic Model of Bonaparte Basin, Australia Northwest Shelf." Journal of Applied Geology 2, no. 2 (2018): 83. http://dx.doi.org/10.22146/jag.39988.

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This research area is located on the Australian NW Shelf close to the westernedge of the Sahul Platform. This research is aimed to generate the palispatic basin model of Bonaparte Basin, Australian Northwest Shelf. It is to predict the impact of Neogene collision on the petroleum system distribution on Australian Northwest Shelf. The main data used in this research are seismic data using qualitative method analysis. The well data is used to well-seismic tied. After data acquisition, the seismic data are interpreted based on the horizon and structure interpretation. These interpretation are to reconstruct the basin evolution thorough geologic time. According to data analysis, the basin evolution palispatic model are divided into Paleo-proterozoic, Paleozoic, Triassic, Early Jurassic, Middle Jurassic, Late Jurassic, Early Cretaceous, Late Cretaceous, Early Eocene, Late Miocene and Recent condition. Regional tectonically there are at least three important events in NW Shelf: Middle Triassic-Jurassic NNE–SSW extension phase, Late Jurassic NE–SW extension phase and the Neogen collision phase; the Neogen collision effects on Northwest Shelf Australia. These three events contributed in forming and disturbing the Paleozoic and Mesozoic petroleum system in Bonaparte basin especially.
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Joo, Ye Eun, Seung Bin Kwon, Yu Jeong Kwon, et al. "Effects of ‘NEOGEN V.BIOME LIPOSOME™’ on the Increased Expression of COL1A1 and HAS2 mRNA in Human Dermal Fibroblasts." Asian Journal of Beauty and Cosmetology 20, no. 4 (2022): 451–59. http://dx.doi.org/10.20402/ajbc.2022.0070.

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Purpose: This study investigated functional cosmetic agent for anti-wrinkle effects of 'NEOGEN V.BIOME LIPOSOME™', which is a liposome in the form of a proprietary technology including a vitamin C active ingredient, on human dermal fibroblasts (HDFs).Methods: The cytotoxicity of 'NEOGEN V.BIOME LIPOSOME™' was measured by performing a water-soluble tetrazolium salt (WST-1) assay. The relative mRNA expression of collagen (<i>COL1A1</i> ) and hyaluronan synthase (<i>HAS2</i>) was measured by quantitative real-time PCR (qRT-PCR) assay.Results: HDF cell viability of 'NEOGEN V.BIOME LIPOSOME™' was no cytotoxic effect at concentrations below 0.25%. The expression of <i>COL1A1</i> and <i>HAS2</i> mRNA was increased in a concentration-dependent manner compared with the negative control group.Conclusion: “NEOGEN V.BIOME LIPOSOME™“ helps to increase collagen and hyaluronan synthase production by promoting <i>COL1A1</i> and <i>HAS2</i> mRNA expression in HDFs; therefore, it is expected to function as an anti-wrinkle cosmetic material.
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Qasim, Syed Saad Bin, Adel A. Al-Asfour, Moosa Abuzayeda, et al. "Differences in Mechanical and Physicochemical Properties of Several PTFE Membranes Used in Guided Bone Regeneration." Materials 16, no. 3 (2023): 904. http://dx.doi.org/10.3390/ma16030904.

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Non-resorbable PTFE membranes are frequently used in dental-guided bone regeneration (GBR). However, there is a lack of detailed comparative studies that define variations among commonly used PTFE membranes in daily dental clinical practice. The aim of this study was to examine differences in physicochemical and mechanical properties of several recent commercial PTFE membranes for dental GBR (CytoplastTM TXT-200, permamem®, NeoGen®, Surgitime, OsseoGuard®-TXT, OsseoGuard®-NTXT). Such differences have been rarely recorded so far, which might be a reason for the varied clinical results. For that reason, we analyzed their surface architecture, chemical composition, tensile strength, Young’s modulus, wettability, roughness, density, thickness and porosity. SEM revealed different microarchitectures among the non-textured membranes; the textured ones had hexagonal indentations and XPS indicated an identical spectral portfolio in all membranes. NeoGen® was determined to be the strongest and OsseoGuard®-TXT was the most elastic. Wettability and roughness were highest for Surgitime but lowest for OsseoGuard®-NTXT. Furthermore, permamem® was the thinnest and NeoGen® was identified as the thickest investigated GBR membrane. The defect volumes and defect volume ratio (%) varied significantly, indicating that permamem® had the least imperfect structure, followed by NeoGen® and then Cytoplast TM TXT-200. These differences may potentially affect the clinical outcomes of dental GBR procedures.
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Huyên, Nguyễn Xuân, Phan Đông Pha, Nguyễn Quốc Cường, and Wysoska Anna. "Some features of Paleogen- Neogen deposits in the Song Lo depression and their relationship with tectonic activities." VIETNAM JOURNAL OF EARTH SCIENCES 25, no. 2 (2018): 150–60. http://dx.doi.org/10.15625/0866-7187/25/2/11896.

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Paleogen- Neogen deposits in the Song Lo depression are continental and consist mainly of course grain size sediments: gravels, pebbles,brecia and course sand in the lower part and fine grain: sandstone, siltstone and argillite in the upper part.Sediment's distribution in the time reflects their rhythm, that characterized for forming condition of braided, anastomosing and meandring rivers.In considering with activities of the Red fault zone, these sediments reflect a period of spreading and lowering with phases of reversing folding. Thestudy area became stable and developed at the end of Neogen epoch.
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Lê, Quang Đạo, Bá Ngọc Nguyễn та Hữu Đạt Nguyễn. "KẾT QUẢ ĐIỀU TRỊ GÃY KÍN KHÔNG VỮNG THÂN XƯƠNG ĐÙI Ở NGƯỜI TRƯỞNG THÀNH BẰNG ĐINH NỘI TỦY NEOGEN TẠI BỆNH VIỆN QUÂN Y 103". VietNam Military Medical Unisversity 50, № 3 (2025): 144–52. https://doi.org/10.56535/jmpm.v50i3.1172.

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Mục tiêu: Đánh giá kết quả điều trị gãy kín không vững thân xương đùi ở người trưởng thành bằng đinh nội tủy (ĐNT) Neogen. Phương pháp nghiên cứu: Nghiên cứu hồi cứu, tiến cứu, mô tả không nhóm chứng trên 40 bệnh nhân (BN) gãy kín thân xương đùi không vững được nắn chỉnh mở và kết xương bên trong bằng ĐNT Neogen tại Bệnh viện Quân y 103 từ tháng 01/2022 - 6/2024. Kết quả: Tuổi trung bình của BN là 45,1 ± 20,8 (18 - 86 tuổi). Nam giới (32 BN = 80,0%) bị tổn thương nhiều hơn nữ giới, tai nạn giao thông (TNGT) là nguyên nhân chủ yếu với 25 BN (62,5%). Phần lớn gãy thân xương đùi loại A với 25/40 BN (62,5%), trong đó, gãy loại A1 và A2 là chủ yếu. Gãy chéo vát và gãy có mảnh rời lớn chiếm đa số với 14/40 BN (35%) mỗi loại. Tất cả các ổ gãy đều liền xương sau 12 tháng, kết quả phục hồi chức năng (PHCN): 87,5% đạt rất tốt, 22,5% đạt tốt. Có 01/40 BN (2,5%) nhiễm khuẩn nông, không có biến chứng nhiễm khuẩn sâu, chậm liền xương và khớp giả. Kết luận: Phương pháp kết xương đùi bằng ĐNT có chốt Neogen mang lại kết quả khả quan, là lựa chọn phù hợp trong điều trị gãy kín không vững thân xương đùi.
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Faturrakhman, Muhammad Luthfi, Emi Sukiyah, and Jamal. "Geometri dan Sebaran Perlipatan berdasarkan analisis citra Landsat 9 dan TerraSAR-X Daerah Watuputih dan sekitarnya Kabupaten Rembang." Jurnal Geologi dan Sumberdaya Mineral 24, no. 2 (2023): 71–77. http://dx.doi.org/10.33332/jgsm.geologi.v24i2.736.

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Cekungan Air Tanah Watuputih secara fisiografis merupakan bagian dari Zona Antiklinorium Rembang. Zona ini  terdiri dari rangkaian perlipatan en-echelon berarah barat -timur yang terbentuk akibat aktivitas tektonik pada Neogen Akhir. Penelitian terdahulu menyebutkan bahwa struktur geologi memegang peranan penting dalam proses hidrogeologi pada daerah Watuputih.  Analisis penginderaan jauh dengan menggunakan teknik band composite, image fusion dan principal component analysis dapat membantu dalam mengidentifikasi geometri dan deliniasi lipatan di daerah Watuputih dan sekitarnya. Perlipatan di daerah Watuputih tersusun dari batuan sedimen berumur Neogen dengan kondisi telah mengalami deformasi dan pelapukan yang intensif terutama pada satuan batugamping. Geomorfologi daerah Watuputih menunjukan bentuk jajaran perbukitan dengan arah ketinggian kurang dari 400m dan terdiri dari jajaran perbukitan antiklin dan lembah sinklin bearah relatif barat – timur. Perlipatan pada daerah Watuputih diidentifikasi terbentuk akibat Sesar Rembang-Madura-Kangean-Sakala dengan arah barat daya – timur laut.Kata Kunci Geomorfologi, Lipatan, Rembang, Watuputih, Landsat
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Khassanov, F. O., U. Kh Kadyrov, and U. E. Khudzhanazarov. "Flora of cretaceous low mountains of South-Western Hissar Ridge." Проблемы ботаники Южной Сибири и Монголии 22, no. 2 (2023): 391–97. http://dx.doi.org/10.14258/pbssm.2023164.

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List of creataceuos flora of Southern-Western Hissar district belonging to Bactrian subprovince of Mountainous Middle Asiatic (Afghan-Turkestan) botanical geographic with 491 species from 250 genera and 49 families of vascular plants province is given. Analysis of florogenitic hypothesis of this florocenotype is also given. We confirmed ideas of R. V. Kamelin (1979) about genesis of this relic subtropical-mediterranean type of vegetation, appeared in paleogen-neogen on the base of relic xeropphytic and partly Mediterranean floras. Flora of gypsaceous low mountains seems to be rather poor and isolated from red cretaceous and green clays presents relic shard of tropical-subtropic afro-arabian flora. First complex is presented by such genera as Plocama Aiton, Molucella, Camptoloma Benth., Rorida J. F.Gmel. having distribution from Canary Islands, Western and Eastern Africa and Sokotra Island to Khorassan and Southern Pamir-Alay. Second complex of gypsaceous mountains presented by autochthonous neogen afghan-pamir-alayan endemic species of genera Spryginia Popov, Bolbosaponaria Bondar., Gypsophila L.
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GUERINI, MICHAEL N., TERRANCE M. ARTHUR, STEVEN D. SHACKELFORD, and MOHAMMAD KOOHMARAIE. "Evaluation of Escherichia coli O157:H7 Growth Media for Use in Test-and-Hold Procedures for Ground Beef Processing†." Journal of Food Protection 69, no. 5 (2006): 1007–11. http://dx.doi.org/10.4315/0362-028x-69.5.1007.

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Since the mid-1990s, the beef industry has used a process called test and hold, wherein beef trim and ground beef are tested to keep products contaminated with Escherichia coli O157:H7 out of commerce. Current O157:H7 detection methods rely on a threshold level of bacterial growth for detection, which is dependent on the growth medium used. Twelve media were examined for growth and doubling time: buffered peptone water (BPW), SOC (which contains tryptone, yeast extract, KCl, MgCl2, and glucose), buffered peptone water plus SOC (BPW-SOC), Bacto-NZYM, RapidChek E. coli O157:H7 medium, BioControl EHEC8 culture medium, Neogen Reveal for E. coli O157:H7—Eight Hour medium (Neogen Reveal 8), BAX System medium for E. coli O157:H7 (BAX), BAX System medium for E. coli O157:H7 MP (BAX-MP), modified E. coli broth, nutrient medium, and tryptic soy broth (TSB). All media were tested at 37 or 42°C under static or shaking conditions. The eight media with the highest total CFU per milliliter and most rapid doubling times were BPW-SOC, NZYM, RapidChek, EHEC8, Neogen Reveal 8, BAX, BAX-MP, and TSB. The ability of these eight media to enrich E. coli O157:H7 in ground beef was further evaluated through time-course experiments using immunomagnetic separation. Of these media, TSB was the easiest to prepare, had a wide application base, and was the least expensive. In the test-and-hold process, the normal ratio of medium to product is 1:10. In this study, a 1:3 ratio worked as well as a 1:10 ratio. Processors using test-and-hold procedures could use 1 liter of TSB to enrich for E. coli O157:H7 in a 375-g sample instead of the usual 3.375 liters, thus saving reagents, time, and labor while maintaining accuracy.
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More sources

Dissertations / Theses on the topic "Neogen"

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Rutishauser, Verena. "Das Südtessin im Neogen : zwischen Schuttstrom und Schelfmeer : eine Fazies- und Ablagerungsraumanalyse /." Zürich : [s.n.], 1986. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=7902.

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Wiechmann, Marc Filip. "Albanerpetontidae (Lissamphibia) aus dem Mesozoikum der Iberischen Halbinsel und dem Neogen von Süddeutschland." [S.l.] : [s.n.], 2004. http://www.diss.fu-berlin.de/2004/224/index.html.

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Hernández, Luján Àngel. "Les tortugues (Testudines) del neogen i quaternari de Catalunya (NE de la Península Ibèrica)." Doctoral thesis, Universitat Autònoma de Barcelona, 2015. http://hdl.handle.net/10803/381065.

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Es revisa el registre neogen i quaternari de les tortugues terrestres i d’aigua dolça (Testudines) de Catalunya, a partir de les restes de la conca del Vallès-Penedès i del pla de Barcelona. A banda d’una revisió bibliogràfica, l’estudi es fonamenta en la descripció i atribució taxonòmica de més de 1.400 restes fòssils (majoritàriament inèdites) procedents de més de 100 localitats. S’emfatitzen aquelles restes que permeten un avenç més significatiu en el coneixement de la sistemàtica, filogènia i/o biostratigrafia de determinats tàxons extints. Respecte a les tortugues terrestres gegants, destaca la descripció dels dos primers cranis coneguts del testudínid Titanchelon richardi (anteriorment Cheirogaster), els quals permeten diferenciar adequadament aquesta espècie de Titanchelon bolivari, l’altre testudínid gegant del Miocè ibèric. Es conclou que, al Vallès-Penedès, el rang estratigràfic de Ti. bolivari (MN3–MN4) no se superposa amb el de Ti. richardi (MN7+8–MN10 i, temptativament, MN6–MN12). El tàxon nominal Cheirogaster arrahonensis és considerat un nomen vanum i el seu holotip atribuït a Testudo (Chersine) sp. També es revisen tots els testudínids de mida més petita presents a la conca del Vallès-Penedès, especialment Testudo (Chersine) catalaunica (MN6–MN9), per a la qual es presenta una diagnosi esmenada i es conclou que no pertany al subgènere extint Paleotestudo. A l’espera d’un estudi més detallat del material disponible, també es reporten nombroses restes inèdites de Testudo del Miocè del Vallès-Penedès, que són atribuïdes a “Paralichelys” catalaunicus [=T. (Chersine) sp. nov., que en el futur necessitarà un nom de reemplaçament per evitar l’homonímia amb T. catalaunica] (MN3–MN4); i Testudo (C.) aff. burgenlandica (MN9–MN11). També es descriu el material clàssic i inèdit de Testudo (Chersine) lunellensis del Plistocè mitjà de Barcelona, una espècie extinta molt propera a l’actual Testudo (Chersine) hermanni. Finalment, es presenta una filogènia revisada de les espècies actuals i extintes de Testudo, que recupera les relacions entre espècies actuals indicades per les dades moleculars, i permet dividir aquest gènere en tres subgèneres actuals i un d’extint. Quant a les tortugues d’aigua dolça, se’n revisa el material publicat i inèdit del Miocè de la conca del Vallès-Penedès. Es reporta per primera vegada la presència dels gèneres Clemmydopsis i Trionyx en aquesta conca, i s’hi constata la presència de diverses espècies de geoemídids pticogasterins del gènere Ptychogaster: Ptychogaster (Temnoclemmys) batalleri (MN6–MN9); P. (Temnoclemmys) sp. (MN3–MN4); i P. (Ptychogaster) sp. (MN4 i MN7+8–MN9). A més, es proporcionen diagnosis esmenades de P. batalleri (de la qual Testudo celonica n’és un sinònim subjectiu posterior), així com dels subgèneres Temnoclemmys i Ptychogaster s.s. En total, es constata la presència 13 espècies de testudins durant el Neogen i el Quaternari de Catalunya, a partir de l’estudi de les restes fòssils del Miocè de la conca del Vallès-Penedès i del Plistocè del pla de Barcelona. Les quelonofaunes del Miocè de Catalunya es caracteritzen per la presència de testudínids terrestres gegants (Titanchelon) i de mida més petita (Testudo), a més de tortugues d’aigua dolça de les famílies dels geoemídids (majoritàriament Ptychogaster, però també Clemmydopsis) i dels trioníquids (Tryonix sp.). Des del Miocè inferior (Ramblià i Aragonià inferior), aquestes faunes de quelonis esdevenen progressivament més riques i menys similars a les de les conques ibèriques internes durant el Miocè mitjà (Aragonià mitjà i superior), fins a assolir un màxim de diversitat en el Miocè superior (Vallesià). A partir d’aquest moment, la diversitat decreix progressivament fins al Turolià, moment a partir del qual no tenim registre fins al Plistocè, en què trobem una quelonofauna empobrida i similar a l’actual, caracteritzada per un testudínid de mida petita (Testudo lunellensis), el geoemídid actual Mauremys, i l’emídid actual Emys.<br>The Neogene and Quaternary record of tortoises and freshwater turtles (Testudines) from Catalonia is revised based on fossil remains from the Vallès-Penedès Basin and the Barcelona Plain. Besides a review of the literature, this study builds on the description and taxonomic attribution of more than 1,400 fossil remains (mostly unpublished) from more than 100 localities. The study emphasizes those remains that enable a significant advance in the systematics, phylogeny and/or biostratigraphy of certain extinct taxa. With regard to giant tortoises, it is noteworthy the description of the two first known skulls of the testudinid Titanchelon richardi (formerly Cheirogaster), which first enable a reliable distinction between this species and Titanchelon bolivari, the other giant testudinid from the Iberian Miocene. It is concluded that, in the Vallès-Penedès, the stratigraphic range of Ti. bolivari (MN3–MN4) does not overlap that of Ti. richardi (MN7+8–MN10 and, tentatively, MN6–MN12). The nominal taxon Cheirogaster arrahonensis is considered a nomen vanum and its holotype assigned to Testudo (Chersine) sp. The smaller testudnids from the Vallès-Penedès Basin are also revised, particularly Testudo (Chersine) catalaunica (MN6–MN9), for which an emended diagnosis is presented, further concluding that it does not belong to the extinct subgenus Paleotestudo. Pending a more detailed study of the available material, numerous additional unpublished remains of other Testudo species from the Miocene of the Vallès-Penedès are reported, being ascribed to “Paralichelys” catalaunicus [=T. (Chersine) sp. nov., which in the future will need a replacement name, so as to avoid homonymy with T. catalaunica] (MN3–MN4); and Testudo (C.) aff. burgenlandica (MN9–MN11). The classical and unpublished material of Testudo (Chersine) lunellensis, an extinct species from the middle Pleistocene of Barcelona very close to the extant Testudo (Chersine) hermanni, is also described. Finally, a revised phylogeny of extant and extinct species of Testudo is provided; it recovers the relationships among extant species as indicated by molecular data, and further enables to distinguish three extant subgenera and one extinct subgenus. Regarding freshwater turtles, the published and unpublished material from the Miocene of the Vallès-Penedès Basin is revised. The presence of genera Clemmydopsis and Trionyx is first reported for this basin, where the presence of several species of ptychogasterine geoemydids is further shown: Ptychogaster (Temnoclemmys) batalleri (MN6–MN9); P. (Temnoclemmys) sp. (MN3–MN4); and P. (Ptychogaster) sp. (MN4 and MN7+8–MN9). Emended diagnoses of P. batalleri (of which Testudo celonica is a junior subjective synonym), as well as of the subgenera Temnoclemmys and Ptychogaster s.s., are further provided. Overall, it is ascertained the presence of 13 species of testunids in the Neogene and Quaternary of Catalonia, on the basis of the study of fossil remains from the Miocene of the Vallès-Penedès Basin and the Pleistocene of the Barcelona Plain. The chelonofaunas from the Miocene of Catalonia are characterized by the presence terrestrial testudinids, both giant (Titanchelon) and smaller (Testudo), as well as that of geoemydid (mostly Ptychogaster, but also Clemmydopsis) and trionychid (Tryonix sp.) freshwater turtles. Since the early Miocene (Ramblian and early Aragonian), these faunas of chelonians have progressively become richer and less similar to those from the inner Iberian basins during the middle Miocene (middle to late Aragonian), until reaching a peak of diversity in the late Miocene (Vallesian). From then onward, their diversity progressively decreases until the Turolian, and there is a gap in the record until the Pleistocene, in which the chelonofauna is impoverished and similar to the living one, being characterized by a small testudinid (Testudo lunellensis), the extant geoemydid Mauremys, and the extant emydid Emys.
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Melnick, Daniel. "Neogene seismotectonics of the south-central Chile margin : subduction-related processes over various temporal and spatial scales." Phd thesis, Potsdam : GeoForschungsZentrum Potsdam, 2007. http://www.gfz-potsdam.de/bib/zbstr.htm.

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Renaudie, Johan. "A synthesis of Antarctic Neogene radiolarians." Doctoral thesis, Humboldt-Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät I, 2014. http://dx.doi.org/10.18452/16985.

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Der Südozean ist die Schlüsselregion zur Kenntnis der neogenen Klimaentwicklung. In diesem Zusammenhang ist die Untersuchung von planktonischen Gemeinschaften in Hinblick auf die Umweltentwicklung von großer Bedeutung. In antarktischen neogenen Sedimenten sind Radiolarien reichlich, in großer Diversität und einheitlich gut erhalten. Sie sind nicht nur perfekte Testobjekte für paläobiologischen Studien, sondern auch eine wichtige Quelle für eine verbesserte Biostratigraphie – bisher behinderte nämlich das Fehlen einer verlässlichen Geochronologie detaillierte Studien. Es wurde ein Datensatz aller Taxa von mehreren Standorten des Südozeans gesammelt: für alle der 98 Proben je ca. 7000 Radiolarien. Die Fauna enthält ca. 500 Arten (inclusive 120 neuer Taxa). Die Untersuchung der Makroevolutionsgeschichte dieser Fauna zeigt, dass eine wesentliche ökologische Umwälzung, ohne Aussterbeereignis, bezogen auf den Verlauf der Artengleichheit und den Anstieg der Gattung Antarctissa, bei ca. 8 Ma erfolgte. Dann, 3 My später, folgte ein wesentlicher Diversitätsverlust. Obwohl das ökologische Ereignis eventuell mit einer Änderung der Primärproduzenten assoziiert sein kann, ist der auslösende Faktor des Diversitätsabfalls unbekannt. Außerdem zeigt der Vergleich zwischen der Diversitätsgeschichte dieser Fauna und einer Paläodiversitätsrekonstruktion südozeanischer Faunen, beruhend auf der Neptune Datenbank, daß der generelle Verläufe mit den Probenteilungsmethodologien nachgezeichnet wird, jedoch diese Methodologien aufgrund grober Verzerrungen nicht geeignet für Detailstudien sind. Schließlich wurde eine biostratigraphische Analyse für die komplette Fauna vom Obermiozän bis Pliozän durchgeführt. Obwohl diese Analyse noch vorlaüfig ist, zeigt sich eine Angleichung des aktuellen Altersmodells um mehr als 1 My. Diese Studie zeigt auch 94 neue, sichere Ereignisse, die für die stratigraphische Einordnung der Antarktischen Sedimente genutzt werden können.<br>The Southern Ocean is the key to understand the Neogene climate evolution. Unfortunately the lack of a robust geochronological framework has hindered precise studies. Equally of interest is understanding how planktonic communities changed in relation with the evolution of these environments. Radiolarians are abundant in Antarctic Neogene sediments, diversified and consistently well-preserved. They should constitute not only an ideal testing ground for paleobiological studies but also a major resource for improved biostratigraphy. In this study, a quantitative, taxonomically-complete dataset have been collected in various sites of the Southern Ocean, using 98 samples and ca. 7000 specimens per sample. Ca. 500 species were uncovered in this fauna, including 120 new to science. The study of the macroevolutionary history of this fauna reveals that a significant, extinctionless ecological turnover, linked to a decrease in the evenness of the species'' abundances and the rise of genus Antarctissa to dominance, occured at ca. 8 Ma, followed 3 My later by a significant diversity loss. Although the ecological event can be tentatively associated with a regional change in the composition of primary producers, the triggering event of the diversity loss is yet to be found. The whole-fauna diversity history was compared to paleodiversity reconstructions computed using subsampling methodologies from the occurrences gathered in the Neptune database. The comparison shows that the main trends are retrieved by the subsampling procedures but also that substantial distortions make them poorly suited for detailed studies. Finally a biostratigraphical analysis was conducted on this whole-fauna dataset for the late Miocene - Pliocene sequence. Although this analysis is still very much preliminary, it shows a coherent readjustement of the current age models by more than 1 My. This study also shows that 94 events seem reliable enough to be used to correlate Southern Ocean sites together.
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Forst, Markus H. "Zur Karbonatsedimentologie, Biofazies und sequenzstratigraphischen Architektur eines fossilen Hochenergie-Schelfs aus dem Neogen der Algarve (Miozän, Südportugal)." [S.l. : s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=969938292.

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Molinu, Anna Rita. "Microbioerosión en substratos esqueléticos del Neógeno y el Cuaternario marinos del Mediterráneo Occidental." Doctoral thesis, Universitat de Barcelona, 2015. http://hdl.handle.net/10803/396601.

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Las perforaciones producidas por microorganismos endolíticos (bacterias, algas, hongos, entre otros) se vienen utilizando en el registro fósil para la interpretación paleoambiental de medios marinos. Las características particulares de estos organismos y de sus trazas permiten identificar zonas fóticas, que a su vez se pueden relacionar con la paleobatimetría relativa. Además, algunas microperforaciones o asociaciones de ellas se utilizan como indicadores paleotermométricos. En la presente memoria se han estudiado mediante técnicas de microscopía electrónica las trazas de microperforación presentes en conchas de moluscos y braquiópodos de edades plioceno y pleistoceno. Las primeras (bivalvos y braquiópodos epibentónicos) fueron recolectadas en varias cuencas marinas de la costa mediterránea española (Alt Empordà, Baix Llobregat, Baix Ebre, Cope y Águilas). Las segundas (bivalvos endo y epibentónicos), en los yacimientos submarinos würmienses de la costa catalana. En total se han identificado 30 icnoespecies distintas, de las cuales 26 aparecen en los depósitos pliocenos (9 de autótrofos y 17 de heterótrofos) y 22 en el Pleistoceno (5 y 17). El 60% de las formas identificadas son comunes para las conchas de ambos periodos. Todas estas icnoespecies se han descrito, figurado y comentado. Se ha nominado una icnoespecie nueva para la ciencia del icnogénero Saccomorpha y se proponen otros 3 morfos susceptibles de representar nuevos icnotaxones. La escasez o mala conservación del material ha impedido su nominación formal. Se citan por primera vez 6 microperforaciones (Planobola macrogota, Rhopalia clavigera, Planobola radicatus, Polyactina araneola, Entobia nana, Aurimorpha varia) en depósitos del Plioceno. La abundancia de muestras recolectadas en los depósitos pleistocenos ha permitido la aplicación por primera vez en el registro fósil de índices ecológicos (de diversidad, de afinidad) para la cuantificación y comparación entre las distintas localidades y/o substratos esqueléticos. En ambos ejemplos se han aplicado las zonaciones batimétricas propuestas por diversos autores para la determinación de las profundidades relativas a las cuales se habrían producido las perforaciones. Cabe destacar que se han tenido en cuenta factores tafonómicos para matizar las interpretaciones, que en general indican aguas relativamente bien iluminadas para los depósitos pliocenos y algo menos para los pleistocenos.<br>Endolithic microorganisms (bacteria, algae, fungi, etc.) produce perforations that have been used in the fossil record for paleoenvironmental interpretation of marine deposits. The particular characteristics of these organisms and their traces allow identifying the photic zone, which in turn can be related to the relative palaeobathymetry. Moreover, microboring assemblages are used as indicators of paleotemperature variation. In the present thesis these structures have been studied through electron microscope techniques. Microboring assemblages occur in mollusk and brachiopod shells from many localities of Pliocene and Pleistocene deposits in northeastern Iberian Peninsula (Mediterranean coast). The epibenthic bivalves and brachiopods were firstly collected from various marine basins in the Spanish Mediterranean coast (Alt Emporda, Baix Llobregat, Baix Ebre, Cope and Aguillas). Later, endo and epibenthic bivalves were recovered in offshore in Würm deposits from the Catalan coast (Cabo Cope, Blanes, Delta de l’Ebre and Palamós). Thirty different ichnospecies were identified, described and figured. Twenty-six of them occur in Pliocene deposits (9 autotrophic and 17 heterotrophic) and twenty-two were identified in the Pleistocene (5 and 17). The 60% of the identified ichnotaxa share both periods (Pliocene and Pleistocene). A new icnoapecies belonging to genus Saccomorpha has been defined. Moreover, four other forms have been proposed as new ichnotaxa. However, the poor preservation status of these microborings hasn’t allows providing a formal nomination. Six boring structures have been described for the first time in Pliocene deposits (Planobola macrogota, Rhopalia clavigera, Planobola radicatus, Polyactina araneola, Entobia nana, Aurimorpha varia). The high number of microboring from Pleistocene deposits has allowed us to use ecological index for the first in the fossil record (diversity, affinity). Ecological indexes have been used for measurement and comparison between different locations and / or skeletal substrates. Many authors proposed a bathymetric zonation for each period (Pliocene and Pleistocene) many taking into consideration distribution of microboring assemblages on shells. This thesis has taken into account taphonomic processes which allow to precise palaeoenvironmental interpretations. As a main conclusion ichnoassemblages from Pliocene deposits indicate illuminated waters. In contrast, ichnoassemblages from Pleistocene deposits suggest less illuminated waters.
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Silveira, Rosemery Rocha da. "Bioestratigrafia e paleoecologia de depósitos neógenos e pleistocenos aflorantes na porção central e ocidental da Bacia do Solimões, Estado do Amazonas, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/132294.

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As 93 amostras palinológicas obtidas deste estudo são oriundas de 12 afloramentos relacionados às formações Solimões e Içá, na região de Coari (5 afloramentos) e Alto Solimões (7 afloramentos), Bacia do Solimões, no estado do Amazonas. Este trabalho apresenta os palinomorfos reconhecidos nestes depósitos (incluindo descrições quando necessárias), com registro fotomicrográfico, relativos a 11 taxons de esporos de fungos, 7 algas, 1 escolecodonte, 1 cisto de dinoflagelado, 31 esporos de pteridófitas, 2 grãos de pólen de gimnospermas e 48 grãos de pólens de angiospermas. Perfis compostos foram construídos para os depósitos aflorantes das regiões de Alto Solimões e Coari, com interpretação estratigráfica. A composição da palinoflora em ambas as áreas apresenta contrastes, sendo aquela de Alto Solimões a de menor diversidade, mas com maior abundância, em comparação com a de Coari. Na região do Alto Solimões há documentação de formas como Crassoretitriletes vanraadshooveni, Foveotriletes ornatos, Magnastriatites grandiosus e a ocorrência de um cisto de dinoflagelado, que confirma influência marinha local para a Formação Solimões. Na região de Coari foi verificado predomínio de esporomorfos, evidenciando contexto continental para as formações Solimões e Içá. Palinofósseis guias de zoneamentos palinológicos foram reconhecidos para a região do Alto Solimões, tais como Crassoretitriletes vanraadshooveni, Grimsdalea magnaclavata, Multimarginites vanderhammeni, Diphyes latiusculus, entre outros. A associação dessas formas permitiu posicionar os depósitos da Formação Solimões na região de Tabatinga e Atalaia do Norte entre o Serravaliano e o Tortoniano (Mioceno Médio/ Superior), com correspondência com a Zona Grimsdalea, pré-estabelecida para intervalo coevo da unidade. Para Coari as amostras foram posicionadas no Neomioceno/Plioceno, a partir do reconhecimento da Subzona de Intervalo de Fenestrites longispinisus, ainda que na área este apresente baixa frequência. Ainda na região de Coari são identificados depósitos mais jovens, a partir da presença de Alnipollenites verus, que indica idade Pleistocena.<br>The 93 pollen samples obtained in this study were the result of research 12 outcrops related to Solimões and Içá formations in the region of Coari (5 outcrops) and Alto Solimões (7 outcrops) in the state of Amazonas. This paper presents the recognized palinomorphs (including descriptions when necessary) and photomicrographs of 11 fungal spores, 7 algae, 1 escolecodont, 1 dinoflagellate cyst, 31 fern spores and 48 pollen grains of angiosperms. The composition of palinoflora in both areas shows contrasts with that of the Alto Solimões less diverse, but more abundantly in comparison with the Coari. In the Alto Solimões is no documentation of ways Crassoretitriletes vanraadshooveni, Foveotriletes ornamentos, Magnastriatites grandiosus and the occurrence of a dinoflagellate cyst, confirming local marine influence to the Solimões Formation. In Coari region was verified predominance of esporomorphs, showing the continental context for the Solimões and Içá formations. Guides species of zonal schemes previously proposed were recognized for the Alto Solimões, such as Crassoretitriletes vanraadshooveni, Grimsdalea magnaclavata, Multimarginites vanderhammeni, Diphyes latiusculus, among others. The association of these forms allowed positioning of the deposits of the Solimões Formation in the region of Tabatinga and Atalaia do Norte on the edge of Serravaliano-Tortonian intervals (Miocene Middle and Upper), with correspondence with the Grimsdalea Zone, preset to coeval range of the unit. To Coari samples were placed in Neomioceno / Pliocene, from the recognition Interval Subdivision of Fenestrites longispinisus, although in this area has a low frequency. Still in the region Coari younger deposits are identified from the presence of Alnipollenites verus, which indicates age Pleistocene.
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Warkus, Frank. "Die neogene Hebungsgeschichte der Patagonischen Anden im Kontext der Subduktion eines aktiven Spreizungszentrums." Phd thesis, [S.l. : s.n.], 2002. http://pub.ub.uni-potsdam.de/2002/0024/warkusf.pdf.

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Poore, Heather Rachel. "Neogene epeirogeny and the Iceland Plume." Thesis, University of Cambridge, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.612116.

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Books on the topic "Neogen"

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S, Barash M., and Institut okeanologii im. P.P. Shirshova., eds. Neogen-chetvertichnai͡a︡ paleookeanologii͡a︡: Po mikropaleontologicheskim dannym. "Nauka", 1989.

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P, Baranova I͡U︡, Grinenko O. V, I͡A︡kutskiĭ institut geologicheskikh nauk, International Geological Correlation Programme, and International Union of Geological Sciences., eds. Paleogen i neogen Severo-Vostoka SSSR. I͡A︡kutskiĭ nauch. t͡s︡entr SO AN SSSR, 1989.

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Varnavskiĭ, Vitaliĭ Georgievich. Paleogen i neogen Priamurʹi͡a i Primorʹi͡a. DVO AN SSSR, 1988.

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Varnavskiĭ, Vitaliĭ Georgievich. Paleogen i neogen Priamurʹi͡a︡ i Primorʹi͡a︡. Akademii͡a︡ nauk SSSR, Dalʹnevostochnoe otd-nie, In-t tektoniki i geofiziki, 1988.

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Severo-Vostochnyĭ kompleksnyĭ nauchno-issledovatelʹskiĭ institut (Akademii͡a nauk SSSR), ред. Morskoĭ i kontinentalʹnyĭ neogen Severo-Vostoka SSSR. SVKNII DVO AN SSSR, 1990.

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Severo-Vostochnyĭ kompleksnyĭ nauchno-issledovatelʹskiĭ institut (Akademii͡a nauk SSSR), ред. Kontinentalʹnyĭ paleogen i neogen Severo-Vostoka SSSR. SVKNII DVO AN SSSR, 1988.

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Jurado, María José. Estudi sedimentològic del Neogen de l'àrea de Ciutadella. Consell Insular de Menorca, 1985.

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Atnipov, M. P. Tektonika neogen-chetvertichnogo osadochnogo chekhla dna I͡A︡ponskogo mori͡a︡. "Nauka", 1987.

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Antipov, M. P. Tektonika neogen-chetvertichnogo osadochnogo chekhla dna I͡Aponskogo mori͡a. Nauka, 1987.

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Jude, Radu. Metalogeneza asociată vulcanismului neogen din nord-vestul Munților Oaș. Editura Academiei Republicii Socialiste România, 1986.

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Book chapters on the topic "Neogen"

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Raugel, Pierre-Jean. "Neogen." In Rapid Food Analysis and Hygiene Monitoring. Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-58362-9_30.

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Eberle, Joachim, Bernhard Eitel, Wolf Dieter Blümel, and Peter Wittmann. "Die Formung der Landschaft im Neogen." In Deutschlands Süden - vom Erdmittelalter zur Gegenwart. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-66233-5_5.

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Young, J. R. "Neogene." In Calcareous Nannofossil Biostratigraphy. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4902-0_8.

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Berchiche, Razika, and Mohamed Saïd Guettouche. "Landslide Susceptibility Modeling Using GIS and MAUT Combined with Artificial Neural Network Models; Case of Aghribs Watershed (Neogen Basin of Tizi-Ouzou, Algeria)." In Advances in Science, Technology & Innovation. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-72547-1_12.

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Traverse, Alfred. "Neogene Palynology." In Paleopalynology. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-5610-9_15.

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Rull, Valentí. "Neogene Diversification." In Ecological Studies. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-57612-6_5.

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Joshipura, Mayank, and Sachin Mathur. "Neogene Tyres." In Cases in Corporate Finance. Routledge India, 2024. http://dx.doi.org/10.4324/9781032724478-23.

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Martínez, Sergio, Claudia J. del Río, and Alejandra Rojas. "Neogene Roots." In Biogeography of the Quaternary Molluscs of the Southwestern Atlantic Ocean. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6055-4_4.

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Lindsay, Everett H. "The Setting." In European Neogene Mammal Chronology. Springer US, 1990. http://dx.doi.org/10.1007/978-1-4899-2513-8_1.

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Hugueney, Marguerite, and Michel Ringeade. "Synthesis on the “Aquitanian” Lagomorph and Rodent Faunas of the Aquitaine Basin (France)." In European Neogene Mammal Chronology. Springer US, 1990. http://dx.doi.org/10.1007/978-1-4899-2513-8_10.

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Conference papers on the topic "Neogen"

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Petrova, Elena. "MORPHOLOGY AND MORPHOMETRY OF BURIED NEOGEN-QUATERNARY VALLEYS WITHIN MIDDLE VOLGA AREA." In 21st SGEM International Multidisciplinary Scientific GeoConference Proceedings 2021. STEF92 Technology, 2021. http://dx.doi.org/10.5593/sgem2021/1.1/s01.011.

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Borges, Gustavo Henrique Carvalho, Paula Adriana Grande, and Isaac Romani. "Variabilidade genética do gene da kappa-caseína em gado leiteiro holandês no estado do Paraná." In II Congresso Internacional Interdisciplinar da Uningá. Editora Uningá, 2023. http://dx.doi.org/10.46311/ed.un.20221018193.

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Objetivou-se avaliar o polimorfismo do gene da kappa-caseína (CSN3) em bovinos da raça holandesa no estado do Paraná. Amostras de pelos de 98 vacas foram coletadas e encaminhadas para laboratório Neogen® em que foram realizadas as extrações e amplificações via “biochip” GGP bovine 100K, de acordo com o protocolo próprio. A análise do SNP CSN3_AY380228_13068, referentes ao alelo A e B da kappa-caseína, evidenciou elevada frequência para o alelo B (0,668) em relação ao alelo A (0,332). Este foi o primeiro estudo realizado no estado do Paraná e evidenciou elevado potencial genético do rebanho para a agroindústria de laticínios.
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L. Kheidri, H., B. Khatir, and F. Belfar. "Sidi Aïssa Geodynamic Evolution During Neogen and Its Impact on the Oued Guetrini Field Meso-Cenozoic Petroleum System." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406042.

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Dzublo, A. D., and V. A. Kholodilov. "Reservoir Potential of Daginski Horizon (Neogen) Deposits within Kirinskoye and Yuzhno-Kirinskoye Gascondensate Fields on the Shelf of Sakhalin Island - Modeling of Productive Hydrocarbon Pools." In First Workshop on Far East Hydrocarbons 2011. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144304.

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"Regional Top Seal Capacity Analysis in JS-1 Ridge, Offshore Madura Involving Seal Geometry, Capillary Seal, Hydrofracturing Analysis, and Natural Fracture Modelling." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-252.

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The Early Miocene reefal carbonate of Kujung-1 is the main hydrocarbon reservoir in JS-1 Ridge Area, North East Java Basin. The varying heights of hydrocarbon columns affect the success rate of exploration in Kujung-1 Formation. The shale of Rancak Unit acts as a regional seal of the Kujung-1 Reservoir. This study aims to understand the character, capacity of seal, and its relationship with hydrocarbon column height, to improve the chances of exploration success. The methodology in this study includes estimation of pore pressures, capillary seals, hydrofracturing seals, seal geometry, and natural fractures modeling. The data used in this study include 41 well, laboratory (Mercury Injection capillary pressure, vitrinite reflectance and X-ray diffraction), and 3D seismic data. The pore pressure of Rancak Unit indicates that it is slightly overpressured by loading mechanism. The presence of slight overpressure increases sealing capacity of Rancak Unit to 1.95 MPa or 221 m gas column equivalent. Hydrofracturing seal does not play an important role in Rancak Unit. The seal geometry of Rancak has good to very good qualitative capabilities to hold hydrocarbon in Kujung-1 Reservoir. Present-day stress magnitudes and orientations have been determined from bore-hole breakout, drilling-induced fractures and LOTs from two wells. Interpretation of borehole breakout and drilling-induced tensile shows that average maximum horizontal stress direction is northeast-southwest. The geomechanically model shows that predominant stress regime at KD-1 and KD-3 Wells is normal stressregime. Fracture distribution based on natural fracture modeling is consistent with the percentage of hydrocarbon filling in Kujung-1 Reservoir. However, the fractures are in a stable condition under present-day stress. Based on further analysis, the natural fractures in the Rancak Unit are the main factor affecting the height of the hydrocarbon column in the Kujung-1 Reservoir. The Neogen compressional tectonic period is estimated to be the period of fracture in the study area in critical condition, and leakage occurred in the Kujung-1 Reservoir at that time.
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Satyana, A. H. "The Neogene in Indonesia: The Most Important Period of Geologic Evolution and Formation of Petroleum Resources." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-g-313.

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The Neogene (23 – 2.6 Ma, including Miocene and Pliocene epochs) is a very important period for Indonesian geology. In this period Indonesia got its present configuration and became the main time controlling the geological setting for the occurrences of energy and mineral resources, as well as geologic disasters. There are important differences in the geological evolution of the Neogene between the western and eastern parts of Indonesia. In Western Indonesia, the outline of the evolution is that transgression occurred in all basins with maximum transgression occurred by the end of early Miocene. Then followed by compression and inversion tectonic events as well as regressive sedimentation from the mid-Miocene to the Pliocene in Sumatra, Natuna, Java basins; while deltaic sedimentation characterized the period in eastern Borneo basins. Volcanism became an important element in the Neogene for Sumatra, Java, Lesser Sunda. In Eastern Indonesia, during the Miocene there was drifting of terranes and their syn-drifting sedimentation, then the terranes collided and were fragmented in the Miocene-Pliocene followed by the formation of regional strike-slip faults, subduction rollback, and the opening of the Banda Sea. The period was also characterized by post-collision molassic sedimentation into the foreland basins. These geological events strongly controlled the petroleum system in every basin in Western and Eastern Indonesia. Although some elements of the petroleum system are Paleogene or Pre-Cenozoic in ages, most of the petroleum system processes associated with final trap formation, petroleum generation, migration, accumulation, and preservation of accumulation occurred in the Neogene. The deltaic basins of Kutai and Tarakan in Western Indonesia and the carbonate basins in Eastern Indonesia (Salawati and Banggai) have their proven petroleum system elements and processes within the Neogene period. Thus, studying the geological evolution and its implications for the petroleum system in the Neogene is very important. The knowledge of this can be applied particularly to less explored basins in Indonesia which are geologically analogue to the productive basins.
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Korucu, Ö., N. ö. Sipahioğlu, S. Aktepe, and E. Beng. "Ultra-Derin Deniz Kuyu Verileri ile Orta-Batı Karadeniz Neojen İstifinin Korelasyonu (Correlation of Neogene Sequence in Western-Central Part of Turkish Black Sea Based on Ultra-Deep Well Data)." In 19th International Petroleum and Natural Gas Congress and Exhibition of Turkey. European Association of Geoscientists & Engineers, 2013. http://dx.doi.org/10.3997/2214-4609-pdb.380.68.

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Flores De Dios Mosqueda, Tania, Ezequiel Arturo Isidro, Marcela Arteaga-Cardona, Carlos Fernando Tapia Garcia, and Pedro Silva Lopez. "Development Of The Mexican Field - Samaria Neogene." In SPE International Heavy Oil Conference and Exhibition. Society of Petroleum Engineers, 2014. http://dx.doi.org/10.2118/172875-ms.

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Carminati, E., C. Doglioni, and F. Lenci. "On the Neogene geodynamics of the Mediterranean." In 64th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2002. http://dx.doi.org/10.3997/2214-4609.201405730.

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Farnsworth, Alexander, Tao Su, Robert Spicer, et al. "NO HIGH TIBETAN PLATEAU UNTIL THE NEOGENE." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319129.

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Reports on the topic "Neogen"

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Souther, J. G., and C. J. Yorath. Chapter 10: Neogene Assemblages. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134095.

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Journeay, J. M., and J. van Ulden. Neogene structural elements of northern Cascadia, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209503.

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Souther, J. G. The Ilgachuz Range - a Late Neogene Shield Volcano. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131229.

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Swift, Stephen A., and David A. Ross. Neogene Stratigraphic Development of the Arabian (Persian) Gulf. Defense Technical Information Center, 2001. http://dx.doi.org/10.21236/ada625817.

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Patterson, R. T. Neogene foraminiferal biostratigraphy of the southern Queen Charlotte Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127725.

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Swift, Stephen A. Stratigraphic Development of the Central Persian Gulf During the Neogene. Defense Technical Information Center, 1998. http://dx.doi.org/10.21236/ada341534.

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Roddick, J. C., and J. G. Souther. Geochronology of Neogene Volcanic Rocks in the northern Garibaldi Belt, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122742.

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Fyles, J. G. High Terrace Sediments, Probably of Neogene Age, West-Central Ellesmere Island, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126702.

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Hamilton, T. S., J. Dostal, and J. M. Shaw. An overiew of xenolith-bearing Neogene to Recent volcanics in the northern Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207875.

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Woodsworth, G. J. Neogene To Recent Volcanism Along the East Side of Hecate Strait, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131978.

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