Ghenea, ; lehm and sandy loess at north of the Mures river, resulted by transformation of the alluvial deposits C. Mrazec, in , in paper Comunicare asupra loessului din Romania. Meanwhile, Filipinos are more doubtless than different immigrants to have sturdy English expertise and have much larger college education charges than the overall overseas- and U. After , there have been made few studies concerning the loess and loess- like deposits and there were achieved especially by pedologists N. In these studies, there was an insufficient nutrient consumption of calcium and iron and an inadequate meals intake, particularly of the dairy and fruit teams.
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Besides the extent of earnings, the social integration of migrant employees is such a decisive standards of the access to healthcare. Politicies aiming at bettering the latter should contain organisations working at the local degree, such as the resident committees.
This article argues that the gender politics of information and communication applied sciences impedes the social process of digital empowerment in Taiwanese transnational households. It examines the altering patterns of ICT use of each family member when some family members migrate, and explore how studying to use ICTs for the aim of transnational household communication is extremely gendered.
By conducting 18 in-depth interviews, I look at the accounts offered by the daughters relating to intimacy, ICTs and gendered inequalities in Taiwanese transnational families. I use decreasing digital inequalities to describe that the daughters teach their dad and mom the way to use completely different kinds of ICTs for a fairer distribution of digital assets. Moreover, via two case research of fathers with lower digital literacy, it examines how men distantiate themselves from ICTs to reclaim their masculinity.
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dating dds The U. Census Bureau defines theforeign bornas people who had no U. The foreign-born population includes naturalized citizens, lawful everlasting residents, refugees and asylees, legal nonimmigrantsand individuals residing in the country without authorization. Florov papers— studies in the Black See steppes — and those of C. Bratescu, — which gave the paleosoils stratigraphyc value: the number of the loess layers indicate the number of the glacial periods, and the number of the paleosoils give the number of the interglacial periods.
This map was used like base for the geological map of Romania, scale 1: In the same period, were made analysis on mechanical, chemical and mineralogical composition of the loess, by S.
Gogalniceanu ; M. Popovata.
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Inin Hungary, it was proposed to research the loess types from Europe and to achieve of a map at scale There have been written many papers about the Quaternary period from different subunits of the Romanian Plain, and about loess and loess-like deposits: T. Bandrabur, ; E. Liteanu,, ; E. Liteanu, C. Ghenea, ; Al. Obreja, Besides, it was drawn a map of the quaternary, at scale Liteanu et. All those mentioned above sustained the deluvial dating dds of the loess-like deposits; after deposition, the materials took the loess characteristics, caused by diagenetic processes.
Bandrabur,; Venera Codarcea, C. Ghenea,; C. Ghenea, Venera Codarcea,a. The pedologists made detailed descriptions of some loess — paleosoils sequences: Ana Conea at al. Florea et. Popovat, in Baragan, Dobrogea and Oltenia. Also, there were made the mechanic, chemical and mineralogical studies: N. Cernescu, ; M. Popovat, ; Tatiana Postolache, a.
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Ana Conea achieved the first and the only, since now, PhD thesis in this study area, in our country, about the loess deposits from the Central and South Dobrogea, paper published in The geographical studies were focused on the following directions: - Descriptions of the processes and the microforms developed on loess: P.
Cotet, ; N. Florea, ; T. Morariu, ; T. Morariu, V. Tufescu, ; V. Tufescu, a. Donisa — the Bistrita Valley ; M. Ielenicz — Dobrogea ; N. Sficlea — the Covurlui Platform ; I. Dating dds — the Poiana Nicorasti Piedmont ; G. Valsan — the Romanian Plain a. Bucur, N. Barbu, ; P. Cotet, ; P. Cotet et.
Oprea, A. Contrea, ; Gr. Posea, Popovat, C. Nicolaescu-Plopisor, M. Spirescu, ; archeological studies: Paunescu, Bitiri a. Bally, ; R. Bally, I. Antonescu, ; R. Bally, P. St nescu, ; Vaicum A. Botzan, ; M. Botzan, C. Haret, N. Petrescu, O. Merculiev, ; Dron A. Afterthere have been made few studies concerning the loess and loess- like deposits and there were achieved especially by pedologists N.
Florea, I. Munteanu et. Panaiotu, Sanda Balescu.
The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Stefanescu in and the aeolian origin of the loess was stated for the first time in our country by L. Mrazec, in
From the most important papers, we signaled those by I. Florea and M. Mihalache,who accomplished an pattern of the cycle evolution for the loess and paleosoil sequences. The geologist applied new methods for the research of the loess and loess-like deposits: paleomagnetism Panaiotu et. The knowledge about the loess deposits from Romania is completed with synthesis papers and universitary courses.
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From the synthesis papers we mention: P. EnculescuO. HerşcoviciM. PopovE. Protopopescu-Pache, F. Cr ciun, D. PopescuEm.
Protopopescu-Pache, M. SpirescuM. SpirescuD. TeaciV. Tufescu Demeteror the Quaternary period: I. DonisN. MacaroviciN. Mezarosz Liteanu and his contributors used, for the deposits from the Romanian Plain, only the term loess-like deposits, with different mechanical composition. Ana Conea, Nadia Ghi ulescu, P.
In time, there were made textural analyses for the loess and loess-like deposits from dating dds regions of the country and stated that the loess from Romania is similar, as concern the mechanical composition, with that from Eastern and Central Europe. The main sources of dust were the southern steppes of Russia Mrazec, or the meadows alluvial plains of the narrow rivers Murgoci et.