Titlebook: Sustainability of European Food Quality Schemes; Multi-Performance, S Filippo Arfini,Valentin Bellassen Book 2019 Springer Nature Switzerla

vasospasm

Žaklina Stojanović,Bojan Ristić,Jelena Filipović three depositional sequences. Sequence 1 is a patchily developed and highly variable alluvial plain and saline playa facies assemblage of probable Oligocene age. Sequence 2 comprises fine-grained fluvial sands grading into marginal marine, coastal sabkha-type deposits with some local reefal beds. I

GROSS

Konstadinos Mattas,Efthimia Tsakiridou,Christos Karelakis,Nikolaou Kallirroi,Alexandros Gatsikos,Ioailing during the initial stages of rifting..The Precambrian basement and pre-rift Mesozoic and Eocene cover have been eroded but there is no evidence of doming prior to initial syn-rift sedimentation. The early-rift Abu Zenima Formation of the eastern and central Gulf of Suez together with the equiv

变量

Viet Hoang,An Nguyenistory of the Red Sea in the central coastal area of western Saudi Arabia..Sedimentary rocks outcropping in the coastal plain around Jeddah are subdivided into two major units which both unconformably overlie the Precambrian crystalline basement: the Usfan Formation probably of late Cretaceous to Eo

Intentional

Apichaya Lilavanichakulrom the equations of fluid mechanics, valid on the particle scale, and then integrate these equations in regions sufficiently large to contain a representative mass of all components. In case of multiphase particulate flow, those regions must be much greater than the size of the particles contained

Lacunar-Stroke

Rankle

Edward Majewski,Agata Malak-Rawlikowskatom sediments of the White Sea. We study both the rock-forming (Al, Fe, Mn) and trace elements (Mo, Cr, Ni, Co, Cu, Pb, Cd, and As) by use of a modified method of selective sequential chemical leaching..A spatial distribution of the occurrence forms of these elements in the surface sediments was est

Affirm

戏法

Bother

habitat

Marina Tomić Maksan,Ružica Brečićthe past decades. Since the early work of Kline (1967), experimental investigations on the detailed structure of the turbulent field in boundary layers have revealed the existence of distinctly organized motions. The present research and the recent investigation of Tomkins (2001) are focused mainly