- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Europe
-
Alps
-
Eastern Alps
-
Dinaric Alps (8)
-
-
-
Balkan Peninsula (1)
-
Southern Europe
-
Albania (2)
-
Balkan Mountains (1)
-
Bosnia-Herzegovina
-
Bosnia
-
Banja Luka Bosnia-Herzegovina (2)
-
Sarajevo Bosnia-Herzegovina (1)
-
-
Herzegovina (5)
-
-
Croatia (1)
-
Dinaric Alps (8)
-
Greece
-
Hellenides (1)
-
-
Istria (1)
-
Italy (1)
-
Macedonia (1)
-
Montenegro (2)
-
Serbia (2)
-
Slovenia (1)
-
Vardar Zone (1)
-
Yugoslavia (10)
-
-
Variscides (1)
-
-
Mediterranean region (2)
-
-
commodities
-
construction materials (1)
-
-
elements, isotopes
-
hydrogen (1)
-
metals
-
arsenic (1)
-
copper (1)
-
iron (1)
-
titanium (1)
-
vanadium (1)
-
zinc (1)
-
-
-
fossils
-
Invertebrata
-
Mollusca (1)
-
Protista
-
Foraminifera (4)
-
Radiolaria
-
Osculosida
-
Nassellina (1)
-
-
-
-
-
microfossils (5)
-
Plantae
-
algae
-
nannofossils
-
Nannoconus (1)
-
-
-
-
thallophytes (1)
-
-
geochronology methods
-
(U-Th)/He (1)
-
Ar/Ar (2)
-
fission-track dating (1)
-
paleomagnetism (1)
-
thermochronology (1)
-
-
geologic age
-
Cenozoic
-
Tertiary
-
Neogene
-
Miocene (2)
-
-
Paleogene
-
Paleocene (1)
-
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous (2)
-
Upper Cretaceous
-
Campanian (1)
-
-
-
Jurassic
-
Upper Jurassic (1)
-
-
Triassic
-
Middle Triassic
-
Ladinian (1)
-
-
-
-
Paleozoic
-
Carboniferous
-
Pennsylvanian (1)
-
-
upper Paleozoic (1)
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks
-
pyroclastics
-
tuff (1)
-
-
rhyolites (1)
-
-
-
ophiolite (2)
-
-
metamorphic rocks
-
metamorphic rocks
-
metasedimentary rocks (1)
-
metavolcanic rocks (1)
-
-
ophiolite (2)
-
-
minerals
-
borates (1)
-
carbonates (1)
-
phosphates
-
apatite (1)
-
-
silicates
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
sheet silicates
-
chlorite group
-
chlorite (1)
-
-
clay minerals
-
kaolinite (1)
-
smectite (1)
-
-
illite (2)
-
mica group
-
muscovite (2)
-
-
-
-
-
Primary terms
-
absolute age (3)
-
Cenozoic
-
Tertiary
-
Neogene
-
Miocene (2)
-
-
Paleogene
-
Paleocene (1)
-
-
-
-
clay mineralogy (1)
-
construction materials (1)
-
crust (2)
-
crystal chemistry (1)
-
crystal structure (2)
-
deformation (1)
-
Europe
-
Alps
-
Eastern Alps
-
Dinaric Alps (8)
-
-
-
Balkan Peninsula (1)
-
Southern Europe
-
Albania (2)
-
Balkan Mountains (1)
-
Bosnia-Herzegovina
-
Bosnia
-
Banja Luka Bosnia-Herzegovina (2)
-
Sarajevo Bosnia-Herzegovina (1)
-
-
Herzegovina (5)
-
-
Croatia (1)
-
Dinaric Alps (8)
-
Greece
-
Hellenides (1)
-
-
Istria (1)
-
Italy (1)
-
Macedonia (1)
-
Montenegro (2)
-
Serbia (2)
-
Slovenia (1)
-
Vardar Zone (1)
-
Yugoslavia (10)
-
-
Variscides (1)
-
-
faults (3)
-
folds (1)
-
geochemistry (2)
-
geochronology (1)
-
geophysical methods (1)
-
ground water (2)
-
hydrogen (1)
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks
-
pyroclastics
-
tuff (1)
-
-
rhyolites (1)
-
-
-
Invertebrata
-
Mollusca (1)
-
Protista
-
Foraminifera (4)
-
Radiolaria
-
Osculosida
-
Nassellina (1)
-
-
-
-
-
Mediterranean region (2)
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous (2)
-
Upper Cretaceous
-
Campanian (1)
-
-
-
Jurassic
-
Upper Jurassic (1)
-
-
Triassic
-
Middle Triassic
-
Ladinian (1)
-
-
-
-
metals
-
arsenic (1)
-
copper (1)
-
iron (1)
-
titanium (1)
-
vanadium (1)
-
zinc (1)
-
-
metamorphic rocks
-
metasedimentary rocks (1)
-
metavolcanic rocks (1)
-
-
orogeny (1)
-
paleogeography (4)
-
paleomagnetism (1)
-
Paleozoic
-
Carboniferous
-
Pennsylvanian (1)
-
-
upper Paleozoic (1)
-
-
phase equilibria (1)
-
Plantae
-
algae
-
nannofossils
-
Nannoconus (1)
-
-
-
-
plate tectonics (2)
-
sea-level changes (1)
-
sedimentary rocks
-
carbonate rocks (1)
-
chemically precipitated rocks
-
evaporites
-
salt (1)
-
-
-
clastic rocks
-
bentonite (1)
-
sandstone (1)
-
-
-
sedimentation (3)
-
sediments
-
clastic sediments (1)
-
-
slope stability (2)
-
stratigraphy (7)
-
structural geology (5)
-
tectonics
-
neotectonics (1)
-
-
thallophytes (1)
-
-
sedimentary rocks
-
flysch (2)
-
sedimentary rocks
-
carbonate rocks (1)
-
chemically precipitated rocks
-
evaporites
-
salt (1)
-
-
-
clastic rocks
-
bentonite (1)
-
sandstone (1)
-
-
-
-
sediments
-
sediments
-
clastic sediments (1)
-
-
Bosnia-Herzegovina
Behaviour of redox-sensitive elements (Ti, As, V and Fe) in clay pit samples with and without Al normalization
Assessment of landslides in Bosnia and Herzegovina and Serbia: A Geoscientists Without Borders project
Assessing trace-element mobility during alteration of rhyolite tephra from the Dinaride Lake System using glass-phase and clay-separate laser ablation inductively coupled plasma mass spectrometry
Deciphering the geodynamic evolution of the Dinaric orogen through the study of the ‘overstepping’ Cretaceous successions
The Kosova landslide, Bosnia and Herzegovina
ABSTRACT Final closure of the Neotethys Ocean basin along the Eurasian margin in southeastern Europe during Eocene–Oligocene time was accompanied by upper-crustal extension expressed as a series of low-angle detachments, basins bounded by normal faults, and volcanism. This extensional belt spanned the southern Balkan Peninsula from the Albanides along the southern Adriatic coast in the west to western Anatolia in the east. Despite the widespread occurrence of this phenomenon within the southern Balkan region, similar extension has not previously been observed in association with the Neotethys closure in the Dinarides, which form the western geographic continuation of this orogenic belt, ending in the Austrian Alps in the northwest. The Mid- Bosnian Schist Mountains are a fault-bounded body of greenschist-facies metamorphic rocks located along the paleogeographic margin of the present-day Adria continental block in the Internal Dinarides. We combine low-temperature thermochronometric ages with field observations of kinematic shear sense indicators and demonstrate that the Mid- Bosnian Schist Mountains were exhumed along a normal fault between 43 and 27.5 Ma. The most rapid cooling occurred between ca. 35 and 27 Ma, coincident with a regional-scale magmatic event. These data constitute the first evidence for major extension in the Dinarides contemporaneous with collision between Adria and the Eurasian margin, and they are consistent with removal of a subducting slab during the transition between oceanic subduction and continental collision.
In situ dehydration behavior of veszelyite (Cu,Zn) 2 Zn(PO 4 )(OH) 3 ·2H 2 O: A single-crystal X-ray study
Movement of the Adria microplate is one of the main elements for understanding crustal deformations in the central Mediterranean and central Europe. To study present-day tectonics in Adria and the nature of its boundary relative to those of the Africa and Eurasia plates, three GPS (Global Positioning System) campaigns involving 41 stations were carried out within CRODYN (the Croatian and Slovene Geodynamic Network). Movement of stations derived in the International Terrestrial Reference Frame 1996 (ITRF96) with respect to the permanent ITRF/IGS (International GPS Service) station GRAZ in Austria, located north of the network, and values of the principal strain rates determined on the basis of analytical surface deformation theory suggest that Adria is divided into three different deformation zones (northern, central, and southern). The domain of northeastern Italy moves 5 mm/yr in an east-northeast direction. The stations in southwestern Slovenia move 3–7 mm/yr in a north-northwest direction, whereas those in southern and northeastern Istria move 4–5 mm/yr in a more easterly direction. The greatest movement (8–10 mm/yr) occurs in central Adria between the Gargano zone and the central Dinarides; there, the movement is northeast-oriented. A fragmentation of Adria into subblocks linking the Gragano zone to the central Dinarides cannot be clearly demonstrated. The southeastern part of Adria, along the coastline of Albania, moves 5–7 mm/yr in an almost east-west direction, and eastern Albania moves 6 mm/yr in an east-southeast direction. The permanent ITRF/IGS stations POTS and WTZR in Germany, BOR1 in Poland, and PENC in Hungary demonstrate no significant movement. The movement of the stations discussed here differs very clearly from the known north-west motion of the Africa plate and suggests that Adria is an independent microplate.
Late Paleozoic–Mesozoic tectonics of the Dinarides revisited: Implications from 40 Ar/ 39 Ar dating of detrital white micas
LONGOBARDIAN (MIDDLE TRIASSIC) ENTACTINARIAN AND NASSELLARIAN RADIOLARIA FROM THE DINARIDES OF BOSNIA AND HERZEGOVINA
Thermal stability and vibrational spectra of the sheet borate tuzlaite, NaCa[B 5 O 8 (OH) 2 ]·3H 2 O
Terrain evaluation for peacekeeping with examples from Bosnia Herzegovina
Abstract Geology has influenced military commanders and the outcome of military operations since ancient times. Terrain evaluation was developed in the 1960s and has benefited greatly from recent developments in GIS (geographic information systems). Peacekeeping operations are increasingly becoming a component of armed forces workload. Geologic support based on terrain evaluation principles was provided to the UN and NATO during peacekeeping and humanitarian relief operations in Bosnia Herzegovina. This included assessments of slope stability, seismic hazard, flood risk, groundwater potential, and construction materials. The role of the geologist advising military commanders during peace support operations essentially becomes a hybrid of those roles of military geologists and conventional civilian engineering geologists. As ever, training in the engineering operations of the “client” is essential to delivering a successful product—usually defined as an approximate answer within a very limited time frame rather than a “good” answer late.
GASPÉITE AND ASSOCIATED Ni-RICH MINERALS FROM VEINS IN ALTERED ULTRABASIC ROCKS FROM DUBOŠTICA, BOSNIA AND HERZEGOVINA
Hydrogeological assessments of United Nations bases in Bosnia Hercegovina
Abstract The need to ensure reliable and secure water supply at United Nations bases in Bosnia Hercegovina led to a hydrogeological and water supply reconnaissance (recce) of each base to determine the feasibility of constructing boreholes within the base perimeter. The recce was conducted under full security measures at a time when the armed conflict in central Bosnia was at its fiercest. Fieldwork was severely limited by the ongoing war. Facilities such as generators, vehicle repair yards, and latrines excluded certain areas within the perimeter wire and restricted where boreholes could be sited. Despite the disruption to the infrastructure and government caused by several years of conflict, some site-specific information was obtained. All sites were assessed as having a good potential for ground water. Preliminary well designs were determined. These were accepted and well drillers were deployed to Vitez, Gornji Vakuf, and Tomislavgrad. Following the deployment of the drillers to Bosnia, the author was able to use his experience of the ground to advise during the well construction phase. The author also provided advice on slope stability along parts of the main supply route (MSR) near Prozor and on the location of suitable borrow pits for material to maintain the surface of the MSR near Redoubt Camp. The participation of the Royal Engineer Specialist Advice Team geologist in Operation Grapple continued the tradition of geological input into recent major British army operations such as those in the Falklands, the Gulf, and northern Iraq.