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12 results on '"Ventrice G. A."'

1. Determinants of Erectile Dysfunction Risk in a Large Series of Italian Men Attending Andrology Clinics

Author

Mirone V., Ricci E., Gentile V., Basile Fasolo C., Parazzini F., Calabrese M., Di Cicco G., Goldoni S., Pento C., Scipioni G., Iantorno R., Nicolai M., Tenaglia R. L., Vaggi L., Annese P., Fiorentino V. A. V., Ielapi V., Morrone G., Cozza P. P., Nigro G., Pariano D., Sidari V., Ventrice G. A., Zumbo G., Carrino M., Fedelini P., Cicalese V., Cirillo A., D' Agostino D., FUSCO, FERDINANDO, Di Rienzo A., Izzo P., Varriale O., Maffucci A., Mazzarella F., Palmiera A., Pecoraro S., Russo A., Sorrentino M., Tripodi V., Zito A., Nobile C., Bianchi M., Mofferdin A., Fiordelise S., Granata A. R. M., Irianni G. N., Lusenti C., Maretti C., Maver A., Pescatori E., Barbieri A., Modenini F., Poletti F., Vitali G., Zoli M., Severini G., Scarano P., Basunti G., Bertaccini A., Soli M., Zaganelli S., Tellarini V., Ughi G., Vaccari E., Zenico T., Liguori G., Savoca G., Belgrano E., Capone M., Ciampalini S., Ciciliato S., Bettin A., Bucci S., Buttazzi L., Trombetta C., Alei G., Franco G., Bitelli M., Bulzomì R., Ferro F., Cardella A., Carlomagno G., Casini A., Catarinella M., Corvese F., De Pasquale F., Di Luigi L., Di Trapano M. C., Marchionni L., D'Ottavio G., Travaglia S., Guerani A., La Pera G., Lauretii S., Mazzoni G., Michetti P. M., Nucci G., IMBIMBO, CIRO, Mirone, V., Ricci, E., Gentile, V., Basile Fasolo, C., Parazzini, F., Calabrese, M., Di Cicco, G., Goldoni, S., Pento, C., Scipioni, G., Iantorno, R., Nicolai, M., Tenaglia, R. L., Vaggi, L., Annese, P., Fiorentino, V. A. V., Ielapi, V., Morrone, G., Cozza, P. P., Nigro, G., Pariano, D., Sidari, V., Ventrice, G. A., Zumbo, G., Carrino, M., Fedelini, P., Cicalese, V., Cirillo, A., D' Agostino, D., Fusco, Ferdinando, Di Rienzo, A., Izzo, P., Varriale, O., Maffucci, A., Mazzarella, F., Imbimbo, Ciro, Palmiera, A., Pecoraro, S., Russo, A., Sorrentino, M., Tripodi, V., Zito, A., Nobile, C., Bianchi, M., Mofferdin, A., Fiordelise, S., Granata, A. R. M., Irianni, G. N., Lusenti, C., Maretti, C., Maver, A., Pescatori, E., Barbieri, A., Modenini, F., Poletti, F., Vitali, G., Zoli, M., Severini, G., Scarano, P., Basunti, G., Bertaccini, A., Soli, M., Zaganelli, S., Tellarini, V., Ughi, G., Vaccari, E., Zenico, T., Liguori, G., Savoca, G., Belgrano, E., Capone, M., Ciampalini, S., Ciciliato, S., Bettin, A., Bucci, S., Buttazzi, L., Trombetta, C., Alei, G., Franco, G., Bitelli, M., Bulzomì, R., Ferro, F., Cardella, A., Carlomagno, G., Casini, A., Catarinella, M., Corvese, F., De Pasquale, F., Di Luigi, L., Di Trapano, M. C., Marchionni, L., D'Ottavio, G., Travaglia, S., Guerani, A., La Pera, G., Lauretii, S., Mazzoni, G., Michetti, P. M., and Nucci, G.

Published
2004

6. Calcolosi vescicale gigante

Author

Pirritano, D., primary, Falvo, F., additional, Spasari, A., additional, De Pasquale, M., additional, Talarico, B., additional, Lanza, T., additional, Ventrice, G. A., additional, Martino, L.F., additional, and Lanza, P., additional

Published
1995
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7. "Storms of crustal stress" and AE earthquake precursors.

Author

Gregori, G. P., Poscolieri, M., Paparo, G., De Simone, S., Rafanelli, C., and Ventrice, G.

Subjects
EARTHQUAKE intensity, ACOUSTIC emission
Abstract

Acoustic emission (AE) displays violent paroxysms preceding strong earthquakes, observed within some large area (several hundred kilometres wide) around the epicentre. We call them "storms of crustal stress" or, briefly "crustal storms". A few case histories are discussed, all dealing with the Italian peninsula, and with the different behaviour shown by the AE records in the Cephalonia island (Greece), which is characterized by a different tectonic setting. AE is an effective tool for diagnosing the state of some wide slab of the Earth's crust, and for monitoring its evolution, by means of AE of different frequencies. The same effect ought to be detected being time-delayed, when referring to progressively lower frequencies. This results to be an effective check for validating the physical interpretation. Unlike a seismic event, which involves a much limited focal volume and therefore affects a restricted area on the Earth's surface, a "crustal storm" typically involves some large slab of lithosphere and crust. In general, it cannot be easily reckoned to any specific seismic event. An earthquake responds to strictly local rheological features of the crust, which are eventually activated, and become crucial, on the occasion of a "crustal storm". A "crustal storm" lasts typically few years, eventually involving several destructive earthquakes that hit at different times, at different sites, within that given lithospheric slab. Concerning the case histories that are here discussed, the lithospheric slab is identified with the Italian peninsula. During 1996-1997 a "crustal storm" was on, maybe elapsing until 2002 (we lack information for the period 1998-2001). Then, a quiet period occurred from 2002 until 26 May 2008, when a new "crustal storm" started, and by the end of 2009 it is still on. During the 1996-1997 "storm" two strong earth- quakes occurred (Potenza and Colfiorito) - and (maybe) in 2002 also the Molise earthquake can be reckoned to this "storm". During the "storm", started in 2008, the l'Aquila earthquake occurred. Additional logical analysis envisages the possibility of distinguishing some kind of "elementary" constituents of a "crustal storm", which can be briefly called "crustal substorms". The concept of "storm" and "substorm" is a common logical aspect, which is shared by several phenomena, depending on their common intrinsic and primary logical properties that can be called lognormality and fractality. Compared to a "crustal storm", a "crustal substorm" is likely to be reckoned to some specific seismic event. Owing to brevity purposes, however, the discussion of "substorms" is given elsewhere. AE is an effective tool for monitoring these phenomena, and other processes that are ongoing within the crust. Eventually they result to be precursors of some more or less violent earthquake. It should be stressed, however, that the target of AE monitoring is diagnosing the Earth's crust. In contrast, earthquake prediction implies a much different perspective, which makes sense only by means of more detailed multiparametric monitoring. An AE array can provide real physical information only about the processes that are objectively ongoing inside different and contiguous large slabs of the crust. The purpose is to monitor the stress propagation that crosses different regions, in order to envisage where and when it can eventually trigger a catastrophe of the system. The conclusion is that continental - or planetary - scale arrays of AE monitoring stations, which record a few different AE frequencies, appear to be the likely first step for diagnosing the evolution of local structures preceding an earthquake. On the other hand, as it is well known, the magnitude of the shock is to be related to the elastic energy stored in the focal volume, rather than to the trigger that starts it. [ABSTRACT FROM AUTHOR]

Published
2010
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8. 'Storms of crustal stress' and AE earthquake precursors

Author

Gregori, G. P., Maurizio Poscolieri, Paparo, G., Simone, S., Rafanelli, C., and Ventrice, G.

Subjects
lcsh:GE1-350, lcsh:Geology, Precursori, lcsh:G, lcsh:QE1-996.5, lcsh:Geography. Anthropology. Recreation, Ultrasuoni, lcsh:Environmental technology. Sanitary engineering, Terremoti, lcsh:TD1-1066, lcsh:Environmental sciences
Abstract

Acoustic emission (AE) displays violent paroxysms preceding strong earthquakes, observed within some large area (several hundred kilometres wide) around the epicentre. We call them "storms of crustal stress" or, briefly "crustal storms". A few case histories are discussed, all dealing with the Italian peninsula, and with the different behaviour shown by the AE records in the Cephalonia island (Greece), which is characterized by a different tectonic setting. AE is an effective tool for diagnosing the state of some wide slab of the Earth's crust, and for monitoring its evolution, by means of AE of different frequencies. The same effect ought to be detected being time-delayed, when referring to progressively lower frequencies. This results to be an effective check for validating the physical interpretation. Unlike a seismic event, which involves a much limited focal volume and therefore affects a restricted area on the Earth's surface, a "crustal storm" typically involves some large slab of lithosphere and crust. In general, it cannot be easily reckoned to any specific seismic event. An earthquake responds to strictly local rheological features of the crust, which are eventually activated, and become crucial, on the occasion of a "crustal storm". A "crustal storm" lasts typically few years, eventually involving several destructive earthquakes that hit at different times, at different sites, within that given lithospheric slab. Concerning the case histories that are here discussed, the lithospheric slab is identified with the Italian peninsula. During 1996–1997 a "crustal storm" was on, maybe elapsing until 2002 (we lack information for the period 1998–2001). Then, a quiet period occurred from 2002 until 26 May 2008, when a new "crustal storm" started, and by the end of 2009 it is still on. During the 1996–1997 "storm" two strong earthquakes occurred (Potenza and Colfiorito) – and (maybe) in 2002 also the Molise earthquake can be reckoned to this "storm". During the "storm", started in 2008, the l'Aquila earthquake occurred. Additional logical analysis envisages the possibility of distinguishing some kind of "elementary" constituents of a "crustal storm", which can be briefly called "crustal substorms". The concept of "storm" and "substorm" is a common logical aspect, which is shared by several phenomena, depending on their common intrinsic and primary logical properties that can be called lognormality and fractality. Compared to a "crustal storm", a "crustal substorm" is likely to be reckoned to some specific seismic event. Owing to brevity purposes, however, the discussion of "substorms" is given elsewhere. AE is an effective tool for monitoring these phenomena, and other processes that are ongoing within the crust. Eventually they result to be precursors of some more or less violent earthquake. It should be stressed, however, that the target of AE monitoring is diagnosing the Earth's crust. In contrast, earthquake prediction implies a much different perspective, which makes sense only by means of more detailed multiparametric monitoring. An AE array can provide real physical information only about the processes that are objectively ongoing inside different and contiguous large slabs of the crust. The purpose is to monitor the stress propagation that crosses different regions, in order to envisage where and when it can eventually trigger a catastrophe of the system. The conclusion is that continental – or planetary – scale arrays of AE monitoring stations, which record a few different AE frequencies, appear to be the likely first step for diagnosing the evolution of local structures preceding an earthquake. On the other hand, as it is well known, the magnitude of the shock is to be related to the elastic energy stored in the focal volume, rather than to the trigger that starts it.

9. The seismic sequence in Central Italy (2016-2017). II Problem solving and decision making on geodynamic interpretation

Author

Giovanni, P. Gregori, Paparo, G., Poscolieri, M., Rafanelli, C., Ventrice, G., Garilli, G., Imperatori, L., Lo Castro, F., and Giovanna ZIMATORE

Subjects
seismic catastrophes, geodynamics of Italy and of the Tyrrhenian Sea, warm mud tectonics, the Emilia earthquake, acoustic emission, the Amatrice-Norcia earthquakes
Abstract

The seismic sequence in Central Italy begun in August 2016 and still in progress in the Spring 2017 is a useful experiment in the natural environment, suited to check the effectiveness of AE (acoustic emission) monitoring in order to diagnose the state of the crust preceding an earthquake. It has been envisaged (Gregori, 2016) that seismic catastrophes can be operatively and effectively managed in terms of a 4 level approach. The focus of a previous paper ("paper I") was on the interpretation of AE records. The present paper ("paper II") deals with a geodynamic interpretation of the Italian peninsula. A critical analysis is considered of some different proposed geodynamic models, with no reference to any "generally agreed" paradigmatic scheme. An innovative perspective is thus found on the basis of a "top-down" approach. That is, only a straight application is considered of the fundamental laws of physics applied to a structural model of Italy, independent of the occurrence or not of seismic events. The target is to interpret phenomena in a self-consistent planetary framework. A subsequent paper ("paper III") is focused on the physical meaning and heuristic perspective of some apparently observed seismic (and volcanic) transmigration. Altogether, this approach shows how catastrophe mitigation and management can be practically improved by means of a "humble" and understating realistic approach to observations, also relying on some unprecedented monitoring techniques and by appealing to no preconceived "generally agreed" arbitrary paradigm.

10. A dataset of acoustic measurements from soundscapes collected worldwide during the COVID-19 pandemic

Author

Challéat, S., Farrugia, N., Froidevaux, J. S. P., Gasc, A., Pajusco, N., Abrahams, C. R., Acevedo-Charry, O., Aguiar, L. M. S., Ahlin, Z. R., Aiple, F., Albert, C. H., Alcocer, I., Alves, A. S., Amorim, F., Andrade, L. B., Araújo, P. M., Ascensão, F., Aucoin, S., Bader, E., Balbuena, D., Barbaro, L., Barbier, E., Cortés, E. B., Barrie, L. E., Bartheld, J. L., Bates, H., Baudouin, A., Beason, R. D., Beckmann, C., Beeston, A., Belá, G., Bellisario, K. M., Belshaw, S., Beltrán, J. F., Beltrão-Mendes, R., Bernard, E., Besche, T., Biro, P. A., Boléat, C., Bossaert, M., Bradley, A., Branco, P., Bredewold, W., Briggs, P. A., Briglia-Ferreira, S. R., Buckner, E., Budinski, I., Burens, A., Buxton, R. T., Canavero, A., Cardoso, P., Carrasco-Rueda, F., Caycedo, P. C., Cazaban, F., Cerveira, L. R., Ceuppens, A., Challéat, A., Larrea, A. C., Charbonneau, A., Charnaux, M., Choksi, P., Cibulka, J., Clavijo-Bustos, J., Colón-Piñeiro, Z., Conde, S., Costa, M. J., Cotão, A., Couturier, C., Scarpelli, M. D. A., da Silva, L. P., Davis, T., de Lacoste, N., Deans, S. L., Dentin, S., Deoniziak, K., Dodgin, S. R., dos Santos, I., Draganoiu, T. I., Drolet, B., Duarte, M. H. L., Duarte, G., Dubset, C., Dziock, F., Eldridge, A., Elise, S., Elliott, D. R., Enguehard, A., Esztl, K., Evans, D. M., Ferreira, D. M., Ferreira, S. A. F., Ferreira, D. F., Ferreira, A. M., Fialas, P. C., Foster-Shaner, L., Freitas, B., Friedman, N. R., Fuller, S., Galop, D., Garside, D., Gattus, J., Geoffray, S., Godart, L., Godet, L., Marques, I. G., González-Garca, F., Griesberger, P., Habib, B., Hallet, M. E., Haribal, M. M., Hatlauf, J., Haupert, S., Herrera, J. M., Herzberger, S. E., Oliveira, F. H., Hodder, K. H., Hoecherl, I., Hulme, M. F., Hyland, E., Jacobs, M., Jaiswal, A., Jégou, L., Jones, S., Jourdan, H., Jůnek, T., Khalatbari, L., Khanwilkar, S., Kitson, J. J. N., Korstjens, Amanda H., Krähenbühl-Künzli, K., Lace, N., Laguet, S., Lankau, H., Laranjeiras, T. O., Lauvin, G., Lavin, S., Le Corre, M., León, M., Levenson, J. J., Linhart, P., Linossier, J., Lizcano, D. J., Llusia, D., Lockett, M., Lopes, P. B., Lopes, R. J., López-Bao, J. V., López-Baucells, A., López-Bosch, D., Machado, R. B., Mande, C., Marchais, G., Marcolin, F., Marn Gómez, O. H., Marques, C. B., Marques, J. T., Martin, T., Mata, V., Matheu-Cortada, E., Médoc, V., Miller, K. E., Montagne, B., Moore, A., Moreno, J. M. A., Moreno-Gómez, F. N., Mueller, S., Murillo-Bedoya, D., Naka, L. N., Newton, A. C., Nunes, J. T., Nyssen, P., Marcaigh, F. Ó., O’Connell, D. P., O’Mara, M. T., Ocampo, D., Ouertani, M., Owren, J. O., Paiva, V. H., Paris, S., Parisot, M., Patankar, S., Pereira, J. M., Barreiro, S. P., Peyronnet, C., Philippe, M., Pijanowski, B. C., Pinto, N., Poff, Z., Poppele, J. M., Power, A., Pratt, V., Proppe, D. S., Proulx, R., Prugh, L., Puechmaille, S. J., Puig-Montserrat, X., Quaglietta, L., Quinn, J. E., Quiroga, N. I., Ramos, M., Rasmussen, R., Reckinger, G., Reed, M., Reginster, J., Rivera, V., Rodrigues, C. F., Rodrguez-González, P. M., Rodrguez-Rodrguez, E., Romaine, L., Roos, A. L., Rosa, J., Ross, S. R. P-J., Rouy, Q., Ryser, A. M., Sadhukhan, S., Sandfort, R., Santos, J. M., Savage, D., Schai-Braun, S. C., Scherer-Lorenzen, M., Sebag, M. S., Segurado, P., Serronha, A. M., Shaw, T., Shepherd, B., Sierra-Durán, C., Silva, B. M., Simon, V., Sinclair, P. F., Soto-Navarro, C., Sourdril, A., Sueur, J., Sugai, L. S. M., Tarrant, I. B., Tattersall, F., Templeton, C. N., Thompson, M. E., Todd, M., Tovar-Garca, J. D., Townsend, K., Tuninetti, A., Ullrich, P. A., Vargas Soto, J. S., Vega, K., Ventrice, G., Victor, P. J., Oliveras, J. V., Villén-Pérez, S., Vinet, O., Vivat, A., Vrignault, J., Walton, W. D. J., Watson, C. J., Wearn, O. R., Whyte, D. L., Windsor, F. M., Wu, Y., Xie, S., Puccherelli, I. Z., Zina, V., Silent Cities project consortium, Challéat, S., Farrugia, N., Froidevaux, J. S. P., Gasc, A., Pajusco, N., Abrahams, C. R., Acevedo-Charry, O., Aguiar, L. M. S., Ahlin, Z. R., Aiple, F., Albert, C. H., Alcocer, I., Alves, A. S., Amorim, F., Andrade, L. B., Araújo, P. M., Ascensão, F., Aucoin, S., Bader, E., Balbuena, D., Barbaro, L., Barbier, E., Cortés, E. B., Barrie, L. E., Bartheld, J. L., Bates, H., Baudouin, A., Beason, R. D., Beckmann, C., Beeston, A., Belá, G., Bellisario, K. M., Belshaw, S., Beltrán, J. F., Beltrão-Mendes, R., Bernard, E., Besche, T., Biro, P. A., Boléat, C., Bossaert, M., Bradley, A., Branco, P., Bredewold, W., Briggs, P. A., Briglia-Ferreira, S. R., Buckner, E., Budinski, I., Burens, A., Buxton, R. T., Canavero, A., Cardoso, P., Carrasco-Rueda, F., Caycedo, P. C., Cazaban, F., Cerveira, L. R., Ceuppens, A., Challéat, A., Larrea, A. C., Charbonneau, A., Charnaux, M., Choksi, P., Cibulka, J., Clavijo-Bustos, J., Colón-Piñeiro, Z., Conde, S., Costa, M. J., Cotão, A., Couturier, C., Scarpelli, M. D. A., da Silva, L. P., Davis, T., de Lacoste, N., Deans, S. L., Dentin, S., Deoniziak, K., Dodgin, S. R., dos Santos, I., Draganoiu, T. I., Drolet, B., Duarte, M. H. L., Duarte, G., Dubset, C., Dziock, F., Eldridge, A., Elise, S., Elliott, D. R., Enguehard, A., Esztl, K., Evans, D. M., Ferreira, D. M., Ferreira, S. A. F., Ferreira, D. F., Ferreira, A. M., Fialas, P. C., Foster-Shaner, L., Freitas, B., Friedman, N. R., Fuller, S., Galop, D., Garside, D., Gattus, J., Geoffray, S., Godart, L., Godet, L., Marques, I. G., González-Garca, F., Griesberger, P., Habib, B., Hallet, M. E., Haribal, M. M., Hatlauf, J., Haupert, S., Herrera, J. M., Herzberger, S. E., Oliveira, F. H., Hodder, K. H., Hoecherl, I., Hulme, M. F., Hyland, E., Jacobs, M., Jaiswal, A., Jégou, L., Jones, S., Jourdan, H., Jůnek, T., Khalatbari, L., Khanwilkar, S., Kitson, J. J. N., Korstjens, Amanda H., Krähenbühl-Künzli, K., Lace, N., Laguet, S., Lankau, H., Laranjeiras, T. O., Lauvin, G., Lavin, S., Le Corre, M., León, M., Levenson, J. J., Linhart, P., Linossier, J., Lizcano, D. J., Llusia, D., Lockett, M., Lopes, P. B., Lopes, R. J., López-Bao, J. V., López-Baucells, A., López-Bosch, D., Machado, R. B., Mande, C., Marchais, G., Marcolin, F., Marn Gómez, O. H., Marques, C. B., Marques, J. T., Martin, T., Mata, V., Matheu-Cortada, E., Médoc, V., Miller, K. E., Montagne, B., Moore, A., Moreno, J. M. A., Moreno-Gómez, F. N., Mueller, S., Murillo-Bedoya, D., Naka, L. N., Newton, A. C., Nunes, J. T., Nyssen, P., Marcaigh, F. Ó., O’Connell, D. P., O’Mara, M. T., Ocampo, D., Ouertani, M., Owren, J. O., Paiva, V. H., Paris, S., Parisot, M., Patankar, S., Pereira, J. M., Barreiro, S. P., Peyronnet, C., Philippe, M., Pijanowski, B. C., Pinto, N., Poff, Z., Poppele, J. M., Power, A., Pratt, V., Proppe, D. S., Proulx, R., Prugh, L., Puechmaille, S. J., Puig-Montserrat, X., Quaglietta, L., Quinn, J. E., Quiroga, N. I., Ramos, M., Rasmussen, R., Reckinger, G., Reed, M., Reginster, J., Rivera, V., Rodrigues, C. F., Rodrguez-González, P. M., Rodrguez-Rodrguez, E., Romaine, L., Roos, A. L., Rosa, J., Ross, S. R. P-J., Rouy, Q., Ryser, A. M., Sadhukhan, S., Sandfort, R., Santos, J. M., Savage, D., Schai-Braun, S. C., Scherer-Lorenzen, M., Sebag, M. S., Segurado, P., Serronha, A. M., Shaw, T., Shepherd, B., Sierra-Durán, C., Silva, B. M., Simon, V., Sinclair, P. F., Soto-Navarro, C., Sourdril, A., Sueur, J., Sugai, L. S. M., Tarrant, I. B., Tattersall, F., Templeton, C. N., Thompson, M. E., Todd, M., Tovar-Garca, J. D., Townsend, K., Tuninetti, A., Ullrich, P. A., Vargas Soto, J. S., Vega, K., Ventrice, G., Victor, P. J., Oliveras, J. V., Villén-Pérez, S., Vinet, O., Vivat, A., Vrignault, J., Walton, W. D. J., Watson, C. J., Wearn, O. R., Whyte, D. L., Windsor, F. M., Wu, Y., Xie, S., Puccherelli, I. Z., Zina, V., and Silent Cities project consortium

Abstract

Political responses to the COVID-19 pandemic led to changes in city soundscapes around the globe. From March to October 2020, a consortium of 261 contributors from 35 countries brought together by the Silent Cities project built a unique soundscape recordings collection to report on local acoustic changes in urban areas. We present this collection here, along with metadata including observational descriptions of the local areas from the contributors, open-source environmental data, open-source confinement levels and calculation of acoustic descriptors. We performed a technical validation of the dataset using statistical models run on a subset of manually annotated soundscapes. Results confirmed the large-scale usability of ecoacoustic indices and automatic sound event recognition in the Silent Cities soundscape collection. We expect this dataset to be useful for research in the multidisciplinary field of environmental sciences.

11. [Unusual ultrasonography of scrotal pathology].

Author

Ucciero G, Ventrice GA, Coluccio A, and Catuogno C

Subjects
Adult, Genital Diseases, Male diagnostic imaging, Humans, Male, Ultrasonography, Scrotum diagnostic imaging
Abstract

The potentialities of ultrasonography in scrotal diseases, with help of color-Doppler and angio-power, as well as their sensibility and specificity are discussed presenting three rather rare cases occurred with acute symptoms. It emphasises the utility of emergency scrotal scanning.

Published
2000

12. [Gastric diverticula: case reports].

Author

Tropeano A, Franzè D, Ventrice GA, and Congestrì F

Subjects
Female, Gastroscopy, Male, Radiography, Diverticulum, Stomach diagnostic imaging, Diverticulum, Stomach therapy
Published
1987

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