Daniela Alexandra Popescu

Daniela Alexandra Popescu
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Daniela verified their affiliation via an institutional email.
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Daniela verified their affiliation via an institutional email.
  • PhD
  • Professor (Associate) at Ştefan cel Mare University of Suceava

About

41
Publications
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47
Citations
Introduction
Daniela Alexandra Popescu currently works at the Department of Geography, Stefan cel Mare University of Suceava. Daniela does research in Mineralogy, Petrology and Geology. Their current project is 'Biota in the Tubiphytes-microbial facies'.
Current institution
Ştefan cel Mare University of Suceava
Current position
  • Professor (Associate)
Additional affiliations
September 1993 - September 2015
Ştefan cel Mare University of Suceava
Position
  • Professor (Assistant)

Publications

Publications (41)
Article
Full-text available
During the period 2000-2005, at Adâncata – „Imaş”. Suceava.co, a barrow cemetery dated to the middle Bronze Age, respectively the Komariv (Komarów) civilization, was investigated. To complete the whole image on the Bronze Age community, there were undertaken archaeological excavations also within the contemporary settlement, situated in the place c...
Book
Full-text available
The reasons for a field trip in Romania and Ukraine? The field trip was organized after the 11th edition of the International Symposium on Environmental Quality and Land Use, Suceava, 2017, between 3rd and 4th of June, on the territory of two neighboring countries, Romania and Ukraine. The field trip itinerary was the following: • The first day (J...
Conference Paper
The sedimentary of the Transilvanian Nappes from the northern sector (Rarău Syncline) of the Eastern Carpathians appears only in allochthonous position, consisting of few unitary litostratigraphical members and many isolated blocks sedimented within the Hauterivian - Albian wildflysh of the Bucovinian Nappe. The Triassic sedimentary is almost excl...
Conference Paper
Introduction Triassic deposits outcropping in the North compartment of the Crystalline – Mesozoic Area of the Eastern Carpathians belong to the system of the Median Dacides Nappes (the Central-East-Carpathian Nappes): Infrabucovinian Nappes, SubBucovinian Nappe and Bucovinian Nappe (Săndulescu, 1984). The last one, that has the higest extention, su...
Article
The Piatra Șoimului klippe belongs to the allochtonous sedimentary succession of the Transylvanian Nappes in the Raru Syncline. It is situated on the western flank of the syncline over the Callovian -- Oxfordian jaspers. The identified micropaleotologic association consists of dasycladales, foraminifera, sphynctozoa, echinoderms, etc. which indicat...
Article
Full-text available
Iezer and Bol�t�u lakes are located in the flish mountains and in the Obcina Feredeului, Northern Romanian Carpathians, respectively. The two lakes were first mentioned in a scientific study in 1964, when their origin of landslide dam was originally suggested. but there remains no evidence of the age of these lakes. Through an examination of histor...
Article
Full-text available
Abstract The studied limestone klippe is located in the northern part of the Suceava district, in the East Carpathians. The klippe is made up of massive, sometimes nodular and breccious limestones, mainly red to violet, light grey, yellow and white in colour. Four types of microfacies were separated, namely packed, filament-bearing wackestones, inv...
Article
Full-text available
The mining activity in Iacobeni – Cârlibaba area datesback as far as the XIII-th century, the first documentary certification being before 1241. After 1775 (when Bucovina was annexed like province to the Austrian Empire) Iacobeni –Cârlibaba area was scientifically examined by Austrian geologists.Geologically and structurally, the Gândacu – Suh rzel...
Article
Full-text available
The Transylvanian Nappes belongs to the Central – East – Carpathian Nappes System (the Dacides Medianes) which forms. The Transylvanian Nappes have a superior position in the Carpahian tectonic system that favored their fragmentation in the obduction process and slow gravitational decollement. This process makes difficult to establish the exclusive...
Article
Full-text available
Microfacies of the Triassic limestones in the Izvorul Malului klippe (Rarău Syncline, Transylvanian Nappes, Eastern Carpathians, Romania). Daniela Alexandra POPESCU1, Liviu Gheorghe POPESCU1 Ștefan cel Mare University of Suceava, Geography Department, University street 13, 720229, Romania, danys@atlas.usv.ro The Transylvanian Nappes belongs to t...
Article
Full-text available
The Triassic sedimentary of the Subbucovinian Nappe crops aut in the Valea Putnei tectonic half-window situated in the north of the Moldavian Compartment of the Crystalline – Mesozoic Area. The crops are located in the north of the Suceava district (north of the Eastern Carpathians). The Triassic sedimentary consists of two facies types: a detritic...
Article
Full-text available
Early Triassic carbonate outcrops were studied in the central sector of the Hăghimaș Syncline with regard to stratigraphy, microfacies and facies interpretation.This is the first microfacies study of these deposits. Early Triassic carbonates in the Hăghimaș Syncline are represented by two stratified successions: limestones and dolomites. The limest...
Article
Full-text available
Microfacies of the Middle Triassic carbonates in the Infrabucovinian Nappes (the North compartment of the Crystalline-Mesozoic Area, Eastern Carpathians. The Triassic sedimentary of the Infrabucovinian Nappes crops out in the three quaries: Puciosu, Suhărzelul Mare and Plaiul Ioanei. These crops are located in the north of the Suceava district (nor...
Article
Full-text available
Geology, microfacies and dolomites exploitation in Pârâul Cailor quarry (Fundu moldovei, Suceava district, Eastern Carpathians) and environmental implication. The Triassic dolomites quarry on yhe Cailor brook is situated in the central-north side of Eastern Carpathians; the dolomites quarry is placed administratively on the territory of Fundu Moldo...
Article
Full-text available
The detritic Seisisan of the Bucovinian Nappe (East Carpathians). Petrographical and biostratigraphical aspects. The Triassic sedimentation of the Bucovinian Nappe begins with a detritic level (Seisian) which corresponds to the first marine transgression of the alpine cycle.The grain level are followed by carbonate deposits (Campilian-?Norian) typi...
Article
Full-text available
Resumé Le synclinal marginal extern est une sous-unité de la zone crystalline-mezozoique des Carpathes Orientales. Il est divisé en deux compartiments: le compartiment sud (la région Tulgheș-Hăghimaș) et le compartiment nord (le Massif Rarău). Notre ouvrage se réfère au compartiment nord le Synclinal Rarău-Bretila. Les recherches de terrain et cell...
Article
Full-text available
Geology, exploitation and capitalization of sandstones levels in Adâncata Area (Suceava district). Implication on the lands utilization. The studied area is situated to the south-south east side of Adâncata locality (Suceava district). Morphologically its belong to Dragomirna Plateau (subunit of Suceava Plateau), which corresponds to the Suceava-Si...
Article
Full-text available
Geological study of the massive Hydaspian dolomites of the Hăghimaş Syncline (Bucovinian Nappe, East Carpathians). The massive dolomites represent the carbonate deposits with the largest outcropping area of the Bucovinian Nappe cropping out on the Hăghimaş Syncline flanks. These deposits appear like a most continuous band on the inner flank where t...
Article
Full-text available
Cuvinte cheie: exploatare, halde de steril, poluare, impact, mediu. The manganese exploitation in the Dadu-Iacobeni mining zone (north -west of Suceava District, north of Eastern Carpathians) on the environment. The first documentary certification of the mining activities in Iacobeni area (Suceava district) from the north of the Eastern Carpathians...

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