The Cycle of Anthropic Rural Landscape in Giurgeu Depression. Spatial-Temporal Evolutions
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Geosciences in the 21 Century______
GEOSCIENCES IN THE 21st CENTURY Symposium dedicated to the 80th anniversary of professor Emil Constantinescu EXTENDED ABSTRACTS EDITORS Antoneta Seghedi, Gheorghe Ilinca, Victor Mocanu GeoEcoMar Bucharest, 2019 Organizatori: Sponsorul volumului: GEOSCIENCES IN THE 21ST CENTURY Symposium dedicated to the 80th anniversary of Professor Emil Constantinescu EXTENDED ABSTRACTS EDITORS Antoneta Seghedi, Gheorghe Ilinca, Victor Mocanu GeoEcoMar Bucharest 2019 NATIONAL INSTITUTE OF MARINE GEOLOGY AND GEOECOLOGY – GeoEcoMar – ROMANIA 23-25 Dimitrie Onciul St. 024053 Bucharest Tel./Fax: +40-021-252 30 39 Contact: [email protected] Descrierea CIP a Bibliotecii Naţionale a României Geosciences in the 21st century / editors: Antoneta Seghedi, Victor Mocanu, Gheorghe Ilinca. - Bucureşti : GeoEcoMar, 2019 Conţine bibliografie ISBN 978-606-94742-7-3 I. Seghedi, Antoneta (ed.) II. Mocanu, Victor (ed.) III. Ilinca, Gheorghe (ed.) 55 Cover: Nicoleta Aniţăi © GeoEcoMar 2019 Printed in Romania CONTENTS Foreword..................................................................................................................................................7 Nicolae Anastasiu The energy mix – the key to performance in the 21st century................................................................8 Alexandru Andrăşanu Geoconservation as a new discipline within Geosciences………………………………………………………………….10 Eliza Anton, Mihaela-Carmen Melinte-Dobrinescu Biostratigraphy of the Istria Basin (Nw Black Sea Shelf) based on calcareous nannofossils……………….14 Laurenţiu -
Administraţia Bazinală De Apă Mureş
PLANUL DE MANAGEMENT AL RISCULUI LA INUNDAŢII Administraţia Bazinală de Apă Mureş Planul de Management al Riscului la Inundaţii Administraţia Bazinală de Apă Mureş Planul de Management al Riscului la Inundaţii Administraţia Bazinală de Apă Mureş CUPRINS Abrevieri ................................................................................................................................... 4 Cap. 1: Prezentarea generală a bazinului hidrografic Mureș .................................................. 6 Cap. 2: Riscul la inundaţii în bazinul hidrografic Mureş ....................................................... 14 2.1. Descrierea lucrărilor existente de protecție împotriva inundațiilor ............................. 14 2.2. Descrierea sistemelor existente de avertizare - alarmare şi de răspuns la inundaţii ............................................................................................ 43 2.3. Istoricul inundaţiilor .................................................................................................... 51 2.4. Evenimentele semnificative de inundaţii ..................................................................... 53 2.5. Zone cu risc potențial semnificativ la inundații ........................................................... 55 2.6. Hărți de hazard și hărți de risc la inundații .................................................................. 59 2.7. Indicatori statistici ....................................................................................................... 63 Cap. 3: Descrierea obiectivelor -
Judet Cerc Livrare Localitate KM Aditionali Bucuresti Resedinta Sectorul 1 0 Bucuresti Resedinta Sectorul 2 0 Bucuresti Resedint
Judet Cerc livrare Localitate KM aditionali Bucuresti Resedinta Sectorul 1 0 Bucuresti Resedinta Sectorul 2 0 Bucuresti Resedinta Sectorul 3 0 Bucuresti Resedinta Sectorul 4 0 Bucuresti Resedinta Sectorul 5 0 Bucuresti Resedinta Sectorul 6 0 Ilfov Cerc 1 1 Decembrie 0 Ilfov Cerc 1 Afumati 0 Ilfov Cerc 1 Balotesti 0 Ilfov Cerc 1 Dumbraveni 0 Ilfov Cerc 1 Saftica 0 Ilfov Cerc 1 Berceni 0 Ilfov Cerc 1 Bragadiru 0 Ilfov Cerc 1 Branesti 0 Ilfov Cerc 1 Islaz 0 Ilfov Cerc 1 Pasarea 0 Ilfov Cerc 1 Vadu Anei 0 Ilfov Cerc 1 Buciumeni 0 Ilfov Cerc 1 Buftea 0 Ilfov Cerc 1 Balaceanca 0 Ilfov Cerc 1 Caldararu 0 Ilfov Cerc 1 Cernica 0 Ilfov Cerc 1 Posta 0 Ilfov Cerc 1 Tanganu 0 Ilfov Cerc 1 Chiajna 0 Ilfov Cerc 1 Dudu 0 Ilfov Cerc 1 Rosu 0 Ilfov Cerc 1 Chitila 0 Ilfov Cerc 1 Rudeni 0 Ilfov Cerc 1 Ciolpani 0 Ilfov Cerc 1 Izvorani 0 Ilfov Cerc 1 Luparia 0 Ilfov Cerc 1 Piscu 0 Ilfov Cerc 1 Ciorogarla 0 Ilfov Cerc 1 Darvari 0 Ilfov Cerc 1 Clinceni 0 Ilfov Cerc 1 Olteni 0 Ilfov Cerc 1 Ordoreanu 0 Ilfov Cerc 1 Copaceni 0 Ilfov Cerc 1 Corbeanca 0 Ilfov Cerc 1 Ostratu 0 Ilfov Cerc 1 Petresti 0 Ilfov Cerc 1 Tamasi 0 Ilfov Cerc 1 Buda 0 Ilfov Cerc 1 Cornetu 0 Ilfov Cerc 1 Darasti-Ilfov 0 Ilfov Cerc 1 Creata 0 Ilfov Cerc 1 Dascalu 0 Ilfov Cerc 1 Gagu 0 Ilfov Cerc 1 Runcu 0 Ilfov Cerc 1 Dobroesti 0 Ilfov Cerc 1 Fundeni 0 Ilfov Cerc 1 Domnesti 0 Ilfov Cerc 1 Teghes 0 Ilfov Cerc 1 Dragomiresti-Deal 0 Ilfov Cerc 1 Dragomiresti-Vale 0 Ilfov Cerc 1 Zurbaua 0 Ilfov Cerc 1 Cozieni 0 Ilfov Cerc 1 Ganeasa 0 Ilfov Cerc 1 Moara Domneasca 0 Ilfov Cerc 1 Piteasca 0 Ilfov Cerc -
Niobian Rutile and Its Associations at Jolotca, Ditrau Alkaline Intrusive Massif, East Carpathians, Romania
THE PUBLISHING HOUSE GEONOMY OF THE ROMANIAN ACADEMY Review article NIOBIAN RUTILE AND ITS ASSOCIATIONS AT JOLOTCA, DITRAU ALKALINE INTRUSIVE MASSIF, EAST CARPATHIANS, ROMANIA Paulina HIRTOPANU1, Robert J. FAIRHURST2 and Gyula JAKAB3 1Department of Mineralogy, University of Bucharest, 1, Nicolae Balcescu Blv., 010041 Bucharest, RO; 2Technical Laboratory at Lhoist North America, Inc., 3700 Hulen Street, Forth Worth, Texas 76107, US; 3IG Mineral Gheorgheni, Romania Corresponding author: Paulina HIRTOPANU, E-mail: [email protected] Accepted December 17, 2014 The Nb-rutile at Jolotca, situated in Ditrau alkaline intrusive complex occurs as intergrowths with ilmenite, Mn-ilmenite, Fe-pyrophanite and has ferrocolumbite, manganocolumbite, aeshynite-(Ce), aeshynite-(Nd), fergusonite-(Y), euxenite-(Y) and polycrase-(Y) exsolutions. The textural relations in this association show the replacement of niobian rutile by ilmenite and Mn ilmenite. Niobian rutile is the oldest mineral. Ilmenite and Mn-ilmenite occur as lamellar exsolutions in niobian rutile and as veins, and separately, in grains as solid solution with Fe-pyrophanite. The range of Nb2O5 content in Nb rutile varies generally from 2 to 15% wt. Sometimes, the values of Nb2O5 (up to 37.5% wt) are higher than any previously recorded for rutile from alkaline suites, pegmatites and carbonatites, having a chemical composition similar to that of old name „ilmenorutile”. Because of such a big difference in chemical composition, and the different kind of appearances of the two rutiles, they can be separated into two Nb rutile generations. The first niobian rutile (niobian rutile I) formed on old rutile, has low Nb2O5 (10-15wt%), and oscillatory composition. Its composition is characteristically close to stoichiometric TiO2. -
Romanian Journal of MINERAL DEPOSITS
Romanian Journal of MINERAL DEPOSITS continuation of DARI DE SEAMA ALE SEDINTELOR INSTITUTULUI DE GEOLOGIE SI GEOFIZICA COMPTES RENDUS DES SÉANCES DE L’INSTITUT DE GÉOLOGIE ET GÉOPHYSIQUE (2. Zacaminte) Founded 1910 by the Geological Institute of Romania ISSN 1220-5648 VOL. 90 No. 1-2 CONTENT Sergiu DRĂGUŞANU, Călin Gabriel TĂMAŞ New geological data on Văidoaia mining field, Roşia Montană Au-Ag epithermal deposit, Apuseni Mountains, Romania ................................................................................................................ 1 Robert SZABO, Gheorghe C. POPESCU Preliminary data on secondary copper minerals from the Şiglău-Uricani perimeter, Vîlcan Mountains, Romania ................................................................................................................. 19 Paulina HÎRTOPANU, Robert J. FAIRHURST, Gyula JAKAB, Sorin Silviu UDUBAŞA Monazite-(Ce) and its associations from the Ditrau alkaline intrusive massif, East Carpathians, Romania .................................................................................................... .............. 27 Ioan PINTEA, Elena Luisa IATAN The magmatic-hydrothermal history of the β-quartz polymorphs from Roşia Montană dacite inferred by solid-, melt-, and fluid inclusion assemblages ........................................................ 41 Geological Institute of Romania Society of Economic Geology of Romania Bucureşti – 2017 DIRECTORS Dr. Ştefan Marincea, General Director of the Geological Institute of Romania Prof. Dr. Gheorghe Damian, President -
Tabel Atribute RO 11.05.2015
Garda Cod / Validare Justificari eliminare (doar la nivel Id trup ID judet / trup Judet Bazinet C1 C2 C3 C4 Forestiera Nivel risc finala de bazinete /trup) 7 AB-7 Cluj AB Molivis AB-7 Total trup 1 0 0 0 galben 9 AB-9 Cluj AB Miras (Cotul) AB-9 Total trup 1 1 0 0 rosu 10 AB-10 Cluj AB Raul Mic AB-10 Total trup 1 0 0 0 galben 12 AB-12 Cluj AB Martinie (Marginea, Tetu) AB-12 Total trup 0 1 0 0 rosu 14 AB-14 Cluj AB Grosesti AB-14 Total trup 0 1 0 0 rosu 15 AB-15 Cluj AB Brustura AB-15 Total trup 1 0 0 0 galben 16 AB-16 Cluj AB Valea Tonii AB-16 Total trup 1 0 0 0 galben 19 AB-19 Cluj AB Chipesa AB-19 Total trup 1 0 0 0 galben 20 AB-20 Cluj AB Garbova AB-20 Total trup 1 0 0 0 galben 26 AB-26 Cluj AB Boz AB-26 Total trup 0 1 0 0 rosu 27 AB-27 Cluj AB Vingard AB-27 Total trup 0 1 0 0 rosu 29 AB-29 Cluj AB Ungurei AB-29 Total trup 0 1 0 0 rosu 30 AB-30 Cluj AB Gardan AB-30 Total trup 0 1 0 0 rosu 31 AB-31 Cluj AB Ohaba (Valea Mare) AB-31 Total trup 0 1 0 0 rosu 38 AB-38 Cluj AB Cenade AB-38 Total trup 0 1 0 0 rosu 39 AB-39 Cluj AB Tarnava (Tarnava Mare) AB-39 Total trup 0 0 0 0 galben 40 AB-40 Cluj AB Lodroman AB-40 Total trup 0 1 0 0 rosu 41 AB-41 Cluj AB Valea Lunga (Tauni) AB-41 Total trup 0 1 0 0 rosu 44 AB-44 Cluj AB Graben AB-44 Total trup 0 1 0 0 rosu 45 AB-45 Cluj AB Spinoasa AB-45 Total trup 1 1 0 1 rosu 46 AB-46 Cluj AB Tatarlaua AB-46 Total trup 1 1 0 1 rosu 48 AB-48 Cluj AB Veseus AB-48 Total trup 1 0 0 0 galben 49 AB-49 Cluj AB Pe Dealul cel mai Departe AB-49 Total trup 1 0 0 0 galben 53 AB-53 Cluj AB Dunarita (Bucerdea) AB-53 Total -
Runoff Potential of Mureş River Upper Basin Tributaries
RUNOFF POTENTIAL OF MUREŞ RIVER UPPER BASIN TRIBUTARIES V. SOROCOVSCHI1, CS.HORVÁTH2 ABSTRACT. – Runoff Potential of Mureş River Upper Basin Tributaries. The upper basin of the Mureş River includes a significant area of the Eastern Carpathians central western part with different runoff formation conditions. In assessing the average annual runoff potential we used data from six gauging stations and made assessments on three distinct periods. Identifying the appropriate areas of the obtained correlations curves (between specific average runoff and catchments mean altitude) allowed the assessment of potential runoff at catchment level and on geographical units. The potential average runoff is also assessed on altitude intervals of the mentioned areas. The runoff potential analysis on hydrographic basins, geographical units and altitude intervals highlights the variant spatial distribution of this general water resources indicator in the different studied areas. Keywords: water resources, Mureş upper basin, geographic units, altitude intervals 1. GENERAL CONSIDERATIONS The upper basin of the Mureş River includes a significant area of the Eastern Carpathians central western part, also known as Moldavo-Transylvanian Carpathians (V. Mihăilescu, 1963). In the study area we find a large part of the Eastern Carpathians neoeruptive chain, represented by the southern slopes of Căliman Mountains, eastern and northern slopes of the Gurghiu Mountains and the northern extremity of the Harghita Mountains (Fig. 1). The runoff formation conditions in the vulcanic chain depend of the neoeruptive relief altitude, which is generally decreasing from north to south, and of the exposure to the advection of western moist air masses. The volcanic relief morphology (cones, craters and plateaus, less represented in the study area) influences only the direction of runoff. -
Lista Localitatilor Din Aria De Acoperire a Curierilor Livrare Gratuita Catre Aceste Localitati La Comenzile Peste 200 De
LISTA LOCALITATILOR DIN ARIA DE ACOPERIRE A CURIERILOR BUCURESTI ALBA Aiud Aiudul De Sus ALBA IULIA Alecus Ampoita Asinip Bacainti Bagau Balcaciu Balomiru De Camp Barabant Beldiu Benic Berghin Beta Blaj Blandiana Boz Bucerdea Bucerdea Granoasa Bucerdea Vinoasa Buninginea Calnic Campul Goblii Capalna Capalna De Jos Captalan Capud Carpenii De Sus Cenade Cergau Cergau Mare Cergau Mic Cetea Ciocasu Cistei Cisteiu De Mures Ciugud Ciugudu De Jos Ciugudu De Sus Ciumbrud Colibi Coslariu Coslariu Nou Craciunelu De Jos Craciunelu De Sus Craiva Cricau Criseni Cunta Cut Daia Romana Dealu Dostatului Dealu Ferului Decea Drambar Drasov Dumbrava (Sasciori) Dumitra Farau Feisa Fenes Galda De Jos Galda De Sus Galtiu Gambas Garbova de Jos Garbova De Sus Garbovita Geoagiu De Sus Geogel Geomal Ghirbom Gura Ariesului Gura Cutului Hapria Hategana Henig Hoparta Ighiel Ighiu Inoc Inuri Isca Izvoarele (Blaj) Izvoarele (Livezi) Jidvei Lancram Laz (Sasciori) Laz (Vintu de Jos) Limba Loman Lunca Ampoitei Lunca Metesului Lunca Tarnavei Lupseni Lupu Magina Magura (Galda De Jos) Manarade Martinie Matacina Medves Mereteu Mesentea Metes Micesti Mihalt Oarda Oarda De Jos Obreja Ocolis Odverem Oiejdea Ormenis Paclisa Padure Padurea Pagida Panade Parau Lui Mihai Patrangeni Petelca Petresti Petrisat Pianu Pianu De Jos Piclisa Pirita Plesi Podu Lui Paul Poiana Ampoiului Poiana Galdei Poiana Ursului Poieni (Blandiana) Poienita (Vintu De Jos) Ponor Posaga De Jos Presaca Ampoiului Purcareti Racatau Rachita Rahau Raicani Ramet Razboieni-Cetate Remetea Rosia De Secas Runc (zlatna) -
The Loss of Villages in Romania After 1990
STUDIA UBB GEOGRAPHIA, LXI, 2, 2016, pp. 101 – 136 (RECOMMENDED CITATION) THE LOSS OF VILLAGES IN ROMANIA AFTER 1990 V. ZOTIC1, DIANA ELENA ALEXANDRU1, LAURA‐MARIA IACOBINIUC1 ABSTRACT. – The Loss of Villages in Romania after 1990. Settlement development is a continuous process significantly influenced by population dynamics. Population decrease through migration and low birth rate has become an issue at European level, and in the case of Romanian rural areas the situation proves even more severe. The aim of our study is to analyse the evolution of rural settlements from emergence to decline based on a seven‐stage development cycle and emphasize on the phenomenon of rural settlement disappearance in Romania after 1990. Results show that even without first‐sight visible or significant effects at national level, the number of rural settlements that have disappeared is continuously increasing, therefore becoming an issue for the development of rural areas. Particularities of the current condition of the built‐up area of each of the analysed villages revealed various levels of destruction from incipient decline (whole built‐up area) to total collapse (very few remains of the built‐up area, and even incorporated in the natural environment). We thus create a typology of disintegrated villages, which are currently found at national level and we reveal their administrative and geographical distribution. We conclude that settlement evolution and the risk of their disappearance should be on the shortlist of priorities of the national policies, strategies and projects designed for the development and planning of rural areas. Keywords: settlement dissapearance, depopulation, evolution stages, typology of dissapeared villages, built‐up area, functional transformation, functionality and decline of human settlement 1. -
Planul De Management Al Riscului La Inundații Mureș
PLANUL DE MANAGEMENT AL RISCULUI LA INUNDAŢII Administraţia Bazinală de Apă Mureș Planul de Management al Riscului la Inundaţii Administraţia Bazinală de Apă Mureş Planul de Management al Riscului la Inundaţii Administraţia Bazinală de Apă Mureş CUPRINS Abrevieri ................................................................................................................................... 4 Cap. 1: Prezentarea generală a bazinului hidrografic Mureș .................................................. 7 Cap. 2: Riscul la inundaţii în bazinul hidrografic Mureș ....................................................... 14 2.1. Descrierea lucrărilor existente de protecție împotriva inundațiilor ............................. 14 2.2. Descrierea sistemelor existente de avertizare - alarmare şi de răspuns la inundaţii ............................................................................................ 43 2.3. Istoricul inundaţiilor .................................................................................................... 51 2.4. Evenimentele semnificative de inundaţii ..................................................................... 53 2.5. Zone cu risc potențial semnificativ la inundații ........................................................... 55 2.6. Hărți de hazard și hărți de risc la inundații .................................................................. 59 2.7. Indicatori statistici ....................................................................................................... 63 Cap. 3: Descrierea obiectivelor -
STATUTUL JUDEŢULUI HARGHITA I. DISPOZIŢII GENERALE Constituţia României a Consacrat Principiul Descentralizării Serviciilor
STATUTUL JUDEŢULUI HARGHITA I. DISPOZIŢII GENERALE Constituţia României a consacrat principiul descentralizării serviciilor publice în unităţile administrativ – teritoriale şi principiul autonomiei locale. În acord cu principiile constituţionale s-a reglementat prin legi organice regimul general al autonomiei locale precum şi organizarea şi funcţionarea autorităţilor administraţiei publice locale, iniţial prin Legea nr. 69/1991 şi mai târziu prin Legea nr. 215/2001 privind administraţia publică locală, cu modificările şi completările ulterioare, ultima reglementare utilizând mai pregnant şi inspirat cadrul constituţional din România. Temeiul legal al elaborării Statutului Judeţului Harghita îl constituie prevederile articolului 20 al Ordonanţei Guvernului nr. 53 din 16 august 2002 privind Statutul cadru al unităţii administrativ teritoriale, modificată şi aprobată prin Legea nr. 96 din 18 martie 2003. Potrivit prevederilor art. 19 din Legea nr. 215/2001 – legea administraţiei publice locale, coroborate cu dispoziţiile art. 5 din Ordonanţa Guvernului nr. 53/2002, Judeţul Harghita ca unitate administrativ - teritorială are calitatea de persoană juridică de drept public. El dispune de un patrimoniu propriu şi capacitate juridică deplină. Judeţul Harghita, ca unitate administrativ-teritorială, poate intra în raporturi juridice cu alte autorităţi sau instituţii publice, cu persoane juridice române sau străine, indiferent de natura acestora, precum şi cu persoane fizice, în condiţiile legii. Judeţul Harghita a fost înfiinţat în anul 1968 când s-a realizat actuala organizare administrativă a teritoriului României, consacrată pe plan juridic prin Legea nr. 2/1968, republicată, cu completările şi modificările ulterioare. După definiţie judeţul este alcătuit din oraşe şi comune, unităţi de bază ale organizării administrativ-teritoriale a ţării, în funcţie de condiţiile geografice, economice şi social - politice, etnice şi de legăturile culturale şi tradiţionale ale populaţiei. -
Relationship from Geology and Radon in Outdoor Air in Massif Ditrău Area, Eastern Carpathians – Romania
Carpathian Journal of Earth and Environmental Sciences, May 2013, Vol. 8, No. 2, p. 163 - 168 RELATIONSHIP FROM GEOLOGY AND RADON IN OUTDOOR AIR IN MASSIF DITRĂU AREA, EASTERN CARPATHIANS – ROMANIA Adriana ION Geological Institute of Romania, Bucharest, 012270, Romania, [email protected] Abstract: Radon activity concentration in outdoor air was measured using alpha radon monitors (Pylon AB- 5 portable with Continuous Passive Radon Detector). Radon in outdoor air was measured in situ, in 5 points, for each lithological unit from the study area. The radon concentration was measured at a height of 15 cm above ground level. The radon exhalation rate was continuously measured for 24 hours with a counting time of 20 minute/interval in each site. The range is considerable: from 2.6 - 52 Bq m-3. The release of radon from rocks and soil is controlled largely by the types of minerals in which uranium and thorium occur. In Ditrău Alkaline Massif, uranium (238U), thorium (232Th) and actinium (235U) are concentrated in accessory minerals such as: zircon, monazite, titanite, allanite, apatite, xenotime, rutile, thorite, bastnäsite, parisite, pyrochlore. Keywords: outdoor radon concentration, passive system, petrography, map 1. INTRODUCTION uranium, thorium in the mineral composition of rocks. Uranium and thorium are concentrated in Radon is a tasteless, odorless, invisible gas accessory minerals (zircon, monazite, titanite, which is the single most important source of natural allanite, apatite, xenotime, thorite, bstnäsite, parisite, radiation to affect the human body (Cosma et al., pyrochlore). 2009). Radon is a naturally occurring radioactive gas In this work, radon in outdoor air was which has three isotopes 222Rn, 220Rn, and 219Rn.