Pub Date : 2023-07-20DOI: 10.24425/agp.2021.137710
Andrzej Kozłowski, Witold Matyszczak
: Kozłowski, A. and Matyszczak, W. 2022. Fluorite and related fluids in the Karkonosze granitoid pluton, SW Poland.
: Kozłowski, A.和Matyszczak, W. 2022。波兰西南部Karkonosze花岗岩体中的萤石及相关流体。
{"title":"Fluorite and related fluids in the Karkonosze granitoid pluton, SW Poland","authors":"Andrzej Kozłowski, Witold Matyszczak","doi":"10.24425/agp.2021.137710","DOIUrl":"https://doi.org/10.24425/agp.2021.137710","url":null,"abstract":": Kozłowski, A. and Matyszczak, W. 2022. Fluorite and related fluids in the Karkonosze granitoid pluton, SW Poland.","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41323709","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2022.142646
Rafał Siuda, A. Januszewska
: Siuda, R. and Januszewska, A. 2022. Recently formed arsenates from an abandoned mine in Radzimowice (SW Poland) and the conditions of their formation. Acta Geologica Polonica , 72 (4), 423–442. Warszawa. In the mining galleries of the abandoned Au-As mine in Radzimowice, diverse groups of secondary arsenates crystallized recently. They form several characteristic assemblages. In the first of them the typical minerals are bukovskýite and melanterite. The second group of secondary arsenates includes scorodite, kaňkite, zýkaite, and pitticite. The third assemblage includes Co-Ni-Mg arsenates of the erythrite-annabergite-hörnesite series. The first assemblage crystallized in a zone with a very high activity of sulphate and arsenate ions and where the pH varies within a narrow range of 2.0–3.5. The second group of secondary arsenates formed in the acidic zone. The minerals identified here suggest pH variation within fairly wide ranges, from about 2.0 to 5.5. Contrary to the first and second mineral assemblage, the Co-Ni-Mg arsenates formed under different geochemical conditions. Their crystallization took place under weak acidic to neutral conditions.
{"title":"Recently formed arsenates from an abandoned mine in Radzimowice (SW Poland) and the conditions of their formation","authors":"Rafał Siuda, A. Januszewska","doi":"10.24425/agp.2022.142646","DOIUrl":"https://doi.org/10.24425/agp.2022.142646","url":null,"abstract":": Siuda, R. and Januszewska, A. 2022. Recently formed arsenates from an abandoned mine in Radzimowice (SW Poland) and the conditions of their formation. Acta Geologica Polonica , 72 (4), 423–442. Warszawa. In the mining galleries of the abandoned Au-As mine in Radzimowice, diverse groups of secondary arsenates crystallized recently. They form several characteristic assemblages. In the first of them the typical minerals are bukovskýite and melanterite. The second group of secondary arsenates includes scorodite, kaňkite, zýkaite, and pitticite. The third assemblage includes Co-Ni-Mg arsenates of the erythrite-annabergite-hörnesite series. The first assemblage crystallized in a zone with a very high activity of sulphate and arsenate ions and where the pH varies within a narrow range of 2.0–3.5. The second group of secondary arsenates formed in the acidic zone. The minerals identified here suggest pH variation within fairly wide ranges, from about 2.0 to 5.5. Contrary to the first and second mineral assemblage, the Co-Ni-Mg arsenates formed under different geochemical conditions. Their crystallization took place under weak acidic to neutral conditions.","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41432251","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2022.140431
P. Pavlishina, D. Dochev, M. Wagreich, V. Koukal
: Pavlishina, P., Dochev, D., Wagreich, M. and Koukal, V. 2023. Integrated biostratigraphy and palaeoenviron-ments of the Upper Cretaceous in the Petrich section (Central Srednogorie Zone, Bulgaria). Acta Geologica Polonica , 73 (1), 33–62. Warszawa. The Upper Cretaceous succession (Coniacian to lowermost Maastrichtian, with focus on the Campanian) at Petrich, Central Srednogorie Zone in Bulgaria, is described and calibrated stratigraphically based on nannofos-sils, dinoflagellate cysts and inoceramids. The following standard nannofossil zones and subzones are identified: UC10–UC11ab (middle to upper Coniacian), UC11c–UC12–UC13 (uppermost Coniacian to Santonian), UC14a (lowermost Campanian), UC14b TP –UC15c TP (lower Campanian to ‘middle’ Campanian), UC15d TP – UC15e TP (upper Campanian), UC16a TP (of Thibault et al . 2016; upper part of the upper Campanian), and UC16b (Campanian–Maastrichtian boundary). The base of the Campanian is defined by the FO of Broinsonia parca parca (Stradner) Bukry, 1969 and Calculites obscurus (Deflandre) Prins and Sissingh in Sissingh, 1977 (a morphotype with a wide central longitudinal suture). The Areoligera coronata dinoflagellate cyst Zone (upper lower Campanian to upper upper Campanian) is identified, corresponding to the UC14b TP –UC16a TP nannofossil subzones. The inoceramid assemblage indicates the ‘ Inoceramus ’ azerbaydjanensis –‘ Inoceramus ’ vorhelmensis Zone, correlated within the interval of nannofossil subzones UC15d TP –UC15e TP . The composition of the dino-flagellate cyst assemblages and palynofacies pattern suggest normal marine, oxic conditions and low nutrient availability within a distal shelf to open marine depositional environment during the Campanian.
{"title":"Integrated biostratigraphy and palaeoenvironments of the Upper Cretaceous in the Petrich section (Central Srednogorie Zone, Bulgaria)","authors":"P. Pavlishina, D. Dochev, M. Wagreich, V. Koukal","doi":"10.24425/agp.2022.140431","DOIUrl":"https://doi.org/10.24425/agp.2022.140431","url":null,"abstract":": Pavlishina, P., Dochev, D., Wagreich, M. and Koukal, V. 2023. Integrated biostratigraphy and palaeoenviron-ments of the Upper Cretaceous in the Petrich section (Central Srednogorie Zone, Bulgaria). Acta Geologica Polonica , 73 (1), 33–62. Warszawa. The Upper Cretaceous succession (Coniacian to lowermost Maastrichtian, with focus on the Campanian) at Petrich, Central Srednogorie Zone in Bulgaria, is described and calibrated stratigraphically based on nannofos-sils, dinoflagellate cysts and inoceramids. The following standard nannofossil zones and subzones are identified: UC10–UC11ab (middle to upper Coniacian), UC11c–UC12–UC13 (uppermost Coniacian to Santonian), UC14a (lowermost Campanian), UC14b TP –UC15c TP (lower Campanian to ‘middle’ Campanian), UC15d TP – UC15e TP (upper Campanian), UC16a TP (of Thibault et al . 2016; upper part of the upper Campanian), and UC16b (Campanian–Maastrichtian boundary). The base of the Campanian is defined by the FO of Broinsonia parca parca (Stradner) Bukry, 1969 and Calculites obscurus (Deflandre) Prins and Sissingh in Sissingh, 1977 (a morphotype with a wide central longitudinal suture). The Areoligera coronata dinoflagellate cyst Zone (upper lower Campanian to upper upper Campanian) is identified, corresponding to the UC14b TP –UC16a TP nannofossil subzones. The inoceramid assemblage indicates the ‘ Inoceramus ’ azerbaydjanensis –‘ Inoceramus ’ vorhelmensis Zone, correlated within the interval of nannofossil subzones UC15d TP –UC15e TP . The composition of the dino-flagellate cyst assemblages and palynofacies pattern suggest normal marine, oxic conditions and low nutrient availability within a distal shelf to open marine depositional environment during the Campanian.","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49628648","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2020.134558
D. Spahić, Zoran Bojić, D. Popović
.
{"title":"Vestiges of Cambro-Ordovician continental accretion in the Carpathian-Balkan orogen: First evidence of the ‘Cenerian event’ in the central Serbo-Macedonian Unit","authors":"D. Spahić, Zoran Bojić, D. Popović","doi":"10.24425/agp.2020.134558","DOIUrl":"https://doi.org/10.24425/agp.2020.134558","url":null,"abstract":".","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46248201","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2022.140429
A. Uchman, Z. Lebanidze, N. Kobakhidze, T. Beridze, Davit Makadze, Koba Lobzhanidze, Sophio Khutsishvili, R. Chagelishvili, K. Koiava, N. Khundadze
: Uchman, A
：Uchman，A
{"title":"Unusual echinoid resting trace records change in the position of the redox boundary (Palaeogene of the Lesser Caucasus in Georgia)","authors":"A. Uchman, Z. Lebanidze, N. Kobakhidze, T. Beridze, Davit Makadze, Koba Lobzhanidze, Sophio Khutsishvili, R. Chagelishvili, K. Koiava, N. Khundadze","doi":"10.24425/agp.2022.140429","DOIUrl":"https://doi.org/10.24425/agp.2022.140429","url":null,"abstract":": Uchman, A","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43632448","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2020.134561
Jun A. Ebersole, D. Cicimurri, Gary L. Stringer
: Ebersole, J.A., Cicimurri, D.J. and Stringer, G.L. 2021. Marine fishes (Elasmobranchii, Teleostei) from the Glendon Limestone Member of the Byram Formation (Oligocene, Rupelian) at site AWa-9, Washington County, Alabama, USA, including a new species of gobiid (Gobiiformes: Gobiidae). Acta Geologica Polonica , 71 (4), 481–518. The Oligocene (Rupelian) Byram Formation (Vicksburg Group) in Alabama, USA, is divided into three members, including (in ascending order) the Glendon Limestone, unnamed marl, and the Bucatunna Clay. The Oligocene marine units in Alabama have been historically under-investigated, but bulk samples recently obtained from Glendon Limestone Member exposures at site AWa-9 in Washington County yielded 20 unequivocal elasmobranch and teleost taxa. This surprisingly diverse paleofauna, based on isolated teeth, bones and otoliths, includes the new taxon, Gobiosoma ? axsmithi sp. nov., as well as “ Aetomylaeus ” sp., Albula sp., Aplodinotus gemma Koken, 1888, Ariosoma nonsector Nolf and Stringer, 2003, Balistidae indet., Citharichthys sp., Myliobatoidei indet., Diretmus ? sp., Hemipristis sp., Negaprion aff. N . gilmorei (Leriche, 1942), Pachyscyllium sp., Paralbula sp., Physogaleus sp., Preophidion meyeri (Koken, 1888), Sciaena pseu-doradians (Dante and Frizzell in Frizzell and Dante, 1965), Sciaenops ? sp., Sparus ? elegantulus Koken, 1888, Sphyraena sp., and Syacium sp. Additional remains were recovered but could not be identified beyond undetermined Elasmobranchii or Teleostei. All these taxa represent first occurrences within the Glendon Limestone Member in Alabama, and the “ Aetomylaeus ” sp., Pachyscyllium sp., Paralbula sp., and Sciaenops ? sp. specimens represent the first occurrences of each in the Oligocene of the Gulf Coastal Plain of the USA. We also report the first record of Oligocene Paralbula Blake, 1940 teeth, and the first occurrence of an Oligocene member of the Balistidae in the Western Hemisphere. This marine vertebrate assemblage indicates that the Glendon Limestone Member at site AWa-9 represented a subtropical to temperate, middle shelf paleoenviron-ment with a paleowater depth interpreted as 30–100 m.
{"title":"Marine fishes (Elasmobranchii, Teleostei) from the Glendon Limestone Member of the Byram Formation (Oligocene, Rupelian) at site AWa-9, Washington County, Alabama, USA, including a new species of gobiid (Gobiiformes: Gobiidae)","authors":"Jun A. Ebersole, D. Cicimurri, Gary L. Stringer","doi":"10.24425/agp.2020.134561","DOIUrl":"https://doi.org/10.24425/agp.2020.134561","url":null,"abstract":": Ebersole, J.A., Cicimurri, D.J. and Stringer, G.L. 2021. Marine fishes (Elasmobranchii, Teleostei) from the Glendon Limestone Member of the Byram Formation (Oligocene, Rupelian) at site AWa-9, Washington County, Alabama, USA, including a new species of gobiid (Gobiiformes: Gobiidae). Acta Geologica Polonica , 71 (4), 481–518. The Oligocene (Rupelian) Byram Formation (Vicksburg Group) in Alabama, USA, is divided into three members, including (in ascending order) the Glendon Limestone, unnamed marl, and the Bucatunna Clay. The Oligocene marine units in Alabama have been historically under-investigated, but bulk samples recently obtained from Glendon Limestone Member exposures at site AWa-9 in Washington County yielded 20 unequivocal elasmobranch and teleost taxa. This surprisingly diverse paleofauna, based on isolated teeth, bones and otoliths, includes the new taxon, Gobiosoma ? axsmithi sp. nov., as well as “ Aetomylaeus ” sp., Albula sp., Aplodinotus gemma Koken, 1888, Ariosoma nonsector Nolf and Stringer, 2003, Balistidae indet., Citharichthys sp., Myliobatoidei indet., Diretmus ? sp., Hemipristis sp., Negaprion aff. N . gilmorei (Leriche, 1942), Pachyscyllium sp., Paralbula sp., Physogaleus sp., Preophidion meyeri (Koken, 1888), Sciaena pseu-doradians (Dante and Frizzell in Frizzell and Dante, 1965), Sciaenops ? sp., Sparus ? elegantulus Koken, 1888, Sphyraena sp., and Syacium sp. Additional remains were recovered but could not be identified beyond undetermined Elasmobranchii or Teleostei. All these taxa represent first occurrences within the Glendon Limestone Member in Alabama, and the “ Aetomylaeus ” sp., Pachyscyllium sp., Paralbula sp., and Sciaenops ? sp. specimens represent the first occurrences of each in the Oligocene of the Gulf Coastal Plain of the USA. We also report the first record of Oligocene Paralbula Blake, 1940 teeth, and the first occurrence of an Oligocene member of the Balistidae in the Western Hemisphere. This marine vertebrate assemblage indicates that the Glendon Limestone Member at site AWa-9 represented a subtropical to temperate, middle shelf paleoenviron-ment with a paleowater depth interpreted as 30–100 m.","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44192269","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2022.143593
{"title":"Seventy years of the Faculty of Geology at the University of Warsaw","authors":"","doi":"10.24425/agp.2022.143593","DOIUrl":"https://doi.org/10.24425/agp.2022.143593","url":null,"abstract":"","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42647730","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2022.142643
W. Alexandrowicz
: Alexandrowicz, W.P. 2023. Application of malacological analysis to reconstruct climate fluctuations and human activity during the Middle and Late Holocene. Research in the valley of the Grajcarek stream (Pieniny Mts., southern Poland). Acta Geologica Polonica , 73 (1), 85–102. Warszawa. The scope of this analysis included fluvial sediments of the low terrace of the Grajcarek stream in the Małe Pieniny Mts. (Western Carpathians). The structure of the terrace has been surveyed in five profiles. The sedi - mentary sequence includes alternating layers of gravel and calcareous mud with a maximum thickness of up to 2.2 m. A rich and varied malacofauna has been found in the mud. The age of the sediments was determined using the radiocarbon method. The sediments that make up the terrace cover the younger part of the Middle Holocene and the entire Late Holocene. The analysis of the malacofauna has allowed for the characterization of environmental changes. The most important of them dates back to the Middle Ages and is associated with the phase of intensive settlement in the Pieniny Mts.. It is indicated by deforestation and the related change in the composition and structure of malacocoenoses manifested by the replacement of forest communities by ones with open-country species. Gravel horizons are records of flood periods correlated with wet climatic phases. It is possible to distinguish six such phases covering the following periods: 6600–6100 y cal BP, 5500–5100 y cal BP, 4500–4100 y cal BP, 3200–2300 y cal BP, 2000–900 y cal BP and 400–200 y cal BP. They correspond to the periods of increased fluvial activity of rivers, intensification of mass movements, advances of alpine glaciers and the increase in the water level in lakes.
:亚历山德罗维兹，W.P. 2023。应用线虫学分析重建全新世中晚期的气候波动和人类活动。在Grajcarek溪谷的研究(波兰南部的Pieniny山)。地质学报，73(1)，85-102。华沙。本分析的范围包括Małe Pieniny山脉(西喀尔巴阡山脉)Grajcarek溪流低阶地的河流沉积物。阶地的构造在五个剖面上进行了测量。沉积层序包括砾石和钙质泥浆交替层，最大厚度可达2.2 m。在泥中发现了丰富多样的malacofafauna。沉积物的年代是用放射性碳法测定的。构成阶地的沉积物覆盖了中全新世的早期和整个晚全新世。对malacofauna的分析使环境变化的特征成为可能。其中最重要的可以追溯到中世纪，与Pieniny mt的密集定居阶段有关。这可以通过森林砍伐和与其相关的malacocoense群落组成和结构的变化来表明，表现为森林群落被开放国家物种取代。砾石层是与潮湿气候阶段相关的洪水时期的记录。可以区分六个这样的阶段，涵盖以下时期:6600-6100 y cal BP, 5500-5100 y cal BP, 4500-4100 y cal BP, 3200-2300 y cal BP, 2000-900 y cal BP和400-200 y cal BP。它们对应的是河流活动增加、群众运动加剧、高山冰川移动和湖泊水位上升的时期。
{"title":"Application of malacological analysis to reconstruct climate fluctuations and human activity during the Middle and Late Holocene. Research in the valley of the Grajcarek stream (Pieniny Mts., southern Poland)","authors":"W. Alexandrowicz","doi":"10.24425/agp.2022.142643","DOIUrl":"https://doi.org/10.24425/agp.2022.142643","url":null,"abstract":": Alexandrowicz, W.P. 2023. Application of malacological analysis to reconstruct climate fluctuations and human activity during the Middle and Late Holocene. Research in the valley of the Grajcarek stream (Pieniny Mts., southern Poland). Acta Geologica Polonica , 73 (1), 85–102. Warszawa. The scope of this analysis included fluvial sediments of the low terrace of the Grajcarek stream in the Małe Pieniny Mts. (Western Carpathians). The structure of the terrace has been surveyed in five profiles. The sedi - mentary sequence includes alternating layers of gravel and calcareous mud with a maximum thickness of up to 2.2 m. A rich and varied malacofauna has been found in the mud. The age of the sediments was determined using the radiocarbon method. The sediments that make up the terrace cover the younger part of the Middle Holocene and the entire Late Holocene. The analysis of the malacofauna has allowed for the characterization of environmental changes. The most important of them dates back to the Middle Ages and is associated with the phase of intensive settlement in the Pieniny Mts.. It is indicated by deforestation and the related change in the composition and structure of malacocoenoses manifested by the replacement of forest communities by ones with open-country species. Gravel horizons are records of flood periods correlated with wet climatic phases. It is possible to distinguish six such phases covering the following periods: 6600–6100 y cal BP, 5500–5100 y cal BP, 4500–4100 y cal BP, 3200–2300 y cal BP, 2000–900 y cal BP and 400–200 y cal BP. They correspond to the periods of increased fluvial activity of rivers, intensification of mass movements, advances of alpine glaciers and the increase in the water level in lakes.","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46550276","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-07-20DOI: 10.24425/agp.2021.139310
{"title":"Reply to the “Discussion”. Oszczypko, N., Oszczypko-Clowes, M. and Olszewska, B. 2020. Geological setting andlithological inventory of the Czarna Woda conglomerates (Magura Nappe, Polish Outer Carpathians). Acta Geologica Polonica, 70, 397–418.","authors":"","doi":"10.24425/agp.2021.139310","DOIUrl":"https://doi.org/10.24425/agp.2021.139310","url":null,"abstract":"","PeriodicalId":7030,"journal":{"name":"Acta Geologica Polonica","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2023-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45673764","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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