Update search
- 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
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
North Africa (1)
-
-
Atlantic Ocean (1)
-
Europe
-
Adriatic region (37)
-
Alps
-
Albanides (1)
-
Eastern Alps
-
Dinaric Alps (3)
-
-
-
Carpathians (1)
-
Central Europe
-
Vienna Basin (2)
-
-
Pyrenees (1)
-
Southern Europe
-
Albania
-
Albanides (1)
-
-
Bulgaria (1)
-
Croatia (12)
-
Dalmatia (3)
-
Dinaric Alps (3)
-
Greece
-
Hellenides (1)
-
Peloponnesus Greece
-
Corinth Greece (1)
-
-
-
Iberian Peninsula
-
Spain (1)
-
-
Ionian Zone (1)
-
Italy
-
Abruzzi Italy (1)
-
Apennines
-
Central Apennines (1)
-
Southern Apennines (1)
-
-
Apulia Italy
-
Gargano (2)
-
-
Emilia-Romagna Italy
-
Romagna (1)
-
-
Marches Italy (2)
-
Molise Italy (1)
-
Po River (1)
-
Sicily Italy (1)
-
Trentino-Alto Adige Italy
-
Trento Italy (1)
-
-
Umbria Italy
-
Perugia Italy
-
Gubbio Italy (1)
-
-
-
Veneto Italy
-
Po Delta (1)
-
Venice Italy (1)
-
-
-
Macedonia (1)
-
Serbia (1)
-
Slovenia (2)
-
Vardar Zone (2)
-
Yugoslavia (2)
-
-
Western Europe
-
France (1)
-
-
-
Mediterranean region (5)
-
Mediterranean Sea
-
East Mediterranean
-
Adriatic Sea (8)
-
Ionian Sea (1)
-
-
West Mediterranean
-
Gulf of Lion (1)
-
-
-
-
commodities
-
bitumens
-
asphalt (1)
-
-
geothermal energy (1)
-
oil and gas fields (2)
-
petroleum
-
natural gas (3)
-
-
-
elements, isotopes
-
carbon
-
C-13/C-12 (6)
-
C-14 (1)
-
-
hydrogen (1)
-
isotope ratios (7)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
-
stable isotopes
-
C-13/C-12 (6)
-
Nd-144/Nd-143 (1)
-
O-18/O-16 (4)
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
Sr-87/Sr-86 (2)
-
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
lead
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
-
nickel (1)
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
-
vanadium (1)
-
-
oxygen
-
O-18/O-16 (4)
-
-
sulfur (2)
-
-
fossils
-
burrows (1)
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (2)
-
-
-
-
Mollusca
-
Bivalvia (2)
-
Cephalopoda
-
Ammonoidea
-
Ammonites (1)
-
-
-
Gastropoda (2)
-
-
Protista
-
Foraminifera
-
Textulariina
-
Lituolacea
-
Orbitolinidae (1)
-
-
-
-
Radiolaria (1)
-
-
-
microfossils (8)
-
palynomorphs (1)
-
Plantae
-
algae
-
calcareous algae (1)
-
Microcodium (1)
-
nannofossils (1)
-
-
-
-
geologic age
-
Anthropocene (1)
-
Cenozoic
-
Quaternary
-
Holocene (2)
-
Pleistocene (1)
-
upper Quaternary (1)
-
-
Tertiary
-
Neogene
-
Miocene
-
middle Miocene
-
Serravallian (1)
-
-
upper Miocene
-
Messinian (2)
-
Tortonian (1)
-
-
-
Pliocene (2)
-
-
Paleogene
-
Eocene (1)
-
Paleocene-Eocene Thermal Maximum (1)
-
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (1)
-
Aptian
-
lower Aptian (1)
-
-
Barremian (1)
-
Hauterivian (2)
-
-
Upper Cretaceous
-
Cenomanian
-
upper Cenomanian (1)
-
-
Coniacian (1)
-
Maestrichtian (1)
-
Santonian (1)
-
Senonian (1)
-
Turonian
-
lower Turonian (1)
-
-
-
-
Jurassic
-
Middle Jurassic (1)
-
-
Maiolica Limestone (1)
-
Triassic
-
Upper Triassic (2)
-
-
-
Paleozoic
-
Permian (2)
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
ultramafics
-
peridotites
-
lherzolite (1)
-
-
-
-
volcanic rocks
-
basalts
-
ocean-island basalts (1)
-
tholeiite (1)
-
-
basanite (1)
-
nephelinite (1)
-
-
-
ophiolite (1)
-
-
metamorphic rocks
-
ophiolite (1)
-
turbidite (1)
-
-
minerals
-
carbonates
-
aragonite (1)
-
-
-
Primary terms
-
absolute age (1)
-
Africa
-
North Africa (1)
-
-
Atlantic Ocean (1)
-
biogeography (1)
-
bitumens
-
asphalt (1)
-
-
carbon
-
C-13/C-12 (6)
-
C-14 (1)
-
-
catalogs (1)
-
Cenozoic
-
Quaternary
-
Holocene (2)
-
Pleistocene (1)
-
upper Quaternary (1)
-
-
Tertiary
-
Neogene
-
Miocene
-
middle Miocene
-
Serravallian (1)
-
-
upper Miocene
-
Messinian (2)
-
Tortonian (1)
-
-
-
Pliocene (2)
-
-
Paleogene
-
Eocene (1)
-
Paleocene-Eocene Thermal Maximum (1)
-
-
-
-
clay mineralogy (1)
-
climate change (4)
-
crust (1)
-
data processing (1)
-
deformation (4)
-
earthquakes (5)
-
Europe
-
Adriatic region (37)
-
Alps
-
Albanides (1)
-
Eastern Alps
-
Dinaric Alps (3)
-
-
-
Carpathians (1)
-
Central Europe
-
Vienna Basin (2)
-
-
Pyrenees (1)
-
Southern Europe
-
Albania
-
Albanides (1)
-
-
Bulgaria (1)
-
Croatia (12)
-
Dalmatia (3)
-
Dinaric Alps (3)
-
Greece
-
Hellenides (1)
-
Peloponnesus Greece
-
Corinth Greece (1)
-
-
-
Iberian Peninsula
-
Spain (1)
-
-
Ionian Zone (1)
-
Italy
-
Abruzzi Italy (1)
-
Apennines
-
Central Apennines (1)
-
Southern Apennines (1)
-
-
Apulia Italy
-
Gargano (2)
-
-
Emilia-Romagna Italy
-
Romagna (1)
-
-
Marches Italy (2)
-
Molise Italy (1)
-
Po River (1)
-
Sicily Italy (1)
-
Trentino-Alto Adige Italy
-
Trento Italy (1)
-
-
Umbria Italy
-
Perugia Italy
-
Gubbio Italy (1)
-
-
-
Veneto Italy
-
Po Delta (1)
-
Venice Italy (1)
-
-
-
Macedonia (1)
-
Serbia (1)
-
Slovenia (2)
-
Vardar Zone (2)
-
Yugoslavia (2)
-
-
Western Europe
-
France (1)
-
-
-
faults (11)
-
folds (3)
-
foliation (1)
-
geochemistry (3)
-
geophysical methods (3)
-
geothermal energy (1)
-
ground water (2)
-
heat flow (1)
-
hydrogen (1)
-
hydrology (2)
-
igneous rocks
-
plutonic rocks
-
ultramafics
-
peridotites
-
lherzolite (1)
-
-
-
-
volcanic rocks
-
basalts
-
ocean-island basalts (1)
-
tholeiite (1)
-
-
basanite (1)
-
nephelinite (1)
-
-
-
inclusions
-
fluid inclusions (1)
-
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (2)
-
-
-
-
Mollusca
-
Bivalvia (2)
-
Cephalopoda
-
Ammonoidea
-
Ammonites (1)
-
-
-
Gastropoda (2)
-
-
Protista
-
Foraminifera
-
Textulariina
-
Lituolacea
-
Orbitolinidae (1)
-
-
-
-
Radiolaria (1)
-
-
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
-
stable isotopes
-
C-13/C-12 (6)
-
Nd-144/Nd-143 (1)
-
O-18/O-16 (4)
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
Sr-87/Sr-86 (2)
-
-
-
land subsidence (2)
-
lava (1)
-
magmas (1)
-
Mediterranean region (5)
-
Mediterranean Sea
-
East Mediterranean
-
Adriatic Sea (8)
-
Ionian Sea (1)
-
-
West Mediterranean
-
Gulf of Lion (1)
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (1)
-
Aptian
-
lower Aptian (1)
-
-
Barremian (1)
-
Hauterivian (2)
-
-
Upper Cretaceous
-
Cenomanian
-
upper Cenomanian (1)
-
-
Coniacian (1)
-
Maestrichtian (1)
-
Santonian (1)
-
Senonian (1)
-
Turonian
-
lower Turonian (1)
-
-
-
-
Jurassic
-
Middle Jurassic (1)
-
-
Maiolica Limestone (1)
-
Triassic
-
Upper Triassic (2)
-
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
lead
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
-
nickel (1)
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
-
vanadium (1)
-
-
metasomatism (1)
-
Mohorovicic discontinuity (1)
-
oil and gas fields (2)
-
orogeny (2)
-
oxygen
-
O-18/O-16 (4)
-
-
paleoclimatology (5)
-
paleoecology (1)
-
paleogeography (5)
-
Paleozoic
-
Permian (2)
-
-
palynomorphs (1)
-
petroleum
-
natural gas (3)
-
-
Plantae
-
algae
-
calcareous algae (1)
-
Microcodium (1)
-
nannofossils (1)
-
-
-
plate tectonics (6)
-
pollution (1)
-
remote sensing (2)
-
sea-level changes (4)
-
sedimentary rocks
-
carbonate rocks
-
dolostone (1)
-
limestone (4)
-
-
chemically precipitated rocks
-
evaporites (1)
-
-
clastic rocks
-
conglomerate (1)
-
sandstone (1)
-
-
-
sedimentary structures
-
biogenic structures
-
bioturbation (1)
-
-
planar bedding structures
-
laminations (2)
-
-
rhizoliths (1)
-
soft sediment deformation
-
slump structures (1)
-
-
-
sedimentation (3)
-
sediments
-
clastic sediments
-
alluvium (1)
-
clay (1)
-
sand (1)
-
-
-
seismology (1)
-
soil mechanics (1)
-
soils (1)
-
stratigraphy (1)
-
structural analysis (2)
-
sulfur (2)
-
tectonics
-
neotectonics (1)
-
-
tectonophysics (2)
-
-
sedimentary rocks
-
calcrete (1)
-
flysch (1)
-
laminite (1)
-
molasse (2)
-
sedimentary rocks
-
carbonate rocks
-
dolostone (1)
-
limestone (4)
-
-
chemically precipitated rocks
-
evaporites (1)
-
-
clastic rocks
-
conglomerate (1)
-
sandstone (1)
-
-
-
turbidite (1)
-
-
sedimentary structures
-
burrows (1)
-
laminite (1)
-
sedimentary structures
-
biogenic structures
-
bioturbation (1)
-
-
planar bedding structures
-
laminations (2)
-
-
rhizoliths (1)
-
soft sediment deformation
-
slump structures (1)
-
-
-
-
sediments
-
sediments
-
clastic sediments
-
alluvium (1)
-
clay (1)
-
sand (1)
-
-
-
turbidite (1)
-
-
soils
-
soils (1)
-
GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Adriatic region
3D active fault kinematic behaviour reveals rapidly alternating near-surface stress states in the Eastern Alps Open Access
Abstract Stress variations in the Earth's crust need to be understood in both the spatial and temporal domains to address a number of pressing societal issues. In this paper, precise three-dimensional records of fault kinematic behaviour obtained by mechanical extensometers are used to investigate changes in stress states along major faults in the Eastern Alps. The monitored faults are fractures with evident Upper Quaternary displacement and are directly attributed to their master tectonic structures. The results demonstrate that activity at the submillimetric scale is highly episodic; periods of repose are punctuated by conspicuous reactivation events affecting one or more of the displacement components. An original approach named the SMB2018 method is used to define the stress state associated with each fault reactivation event. The outputs evidence significant short-term changes in the local stress regime. The directions of the principal normal stresses calculated from these reactivation events present generally similar patterns for both compressional and extensional stress states. Consequently, submillimetric fault activity cannot be controlled by a rotating stress field; such shifts can only be caused by a change in the magnitude of the individual principal normal stresses so that the maximum compression changes to the minimum and vice versa.
Combining Seismotectonic and Catalog‐Based 3D Models for Advanced Smoothed Seismicity Computations Available to Purchase
Tectono-magmatic evolution during the extensional phase of a Wilson Cycle: a review of the Alpine Tethys case and implications for Atlantic-type margins Available to Purchase
The Adriatic Thrust Fault of the 2021 Seismic Sequence Estimated from Accurate Earthquake Locations Using sP Depth Phases Available to Purchase
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary Open Access
Analysis of global navigation satellite system data along the Southern Gas Corridor and estimate of the expected displacements Open Access
The First Very Broadband Mediterranean Network: 30 Yr of Data and Seismological Research Available to Purchase
Provenance studies of amphorae from the Greek colony Pharos on the island of Hvar, Croatia Available to Purchase
ABSTRACT We present the results of a compositional characterization study of amphorae from the ancient Greek town of Pharos, today Stari Grad, on the island of Hvar, in central Dalmatia, Croatia. The aim of the study was to identify the provenance of amphorae unearthed in Pharos, to determine the locally produced amphorae, and to identify the provenance of imported amphorae with a scientific-based approach, using optical thin-section petrography and bulk geochemical analysis by wavelength-dispersive X-ray fluorescence on 19 samples of different types of amphorae and reference materials. The results of the analyses allowed us to identify a group of imported amphorae from Corinth or Corfu and a group of imported amphorae from southern Italy, probably from Calabria. We were also able to identify a third group of imported amphorae from an as-yet-unknown provenance/workshop. Finally, according to the geochemical composition and close match with the reference material, namely, kitchenware, only two amphorae from the examined collection could be identified as local products. The results of the compositional characterization of amphorae from Pharos show us that an ancient Greek town had trade contacts beyond the Adriatic-Ionian region, and they provide opportunities for further studies of ancient amphorae production and circulation in this part of the Mediterranean.
Pelagosite revisited: The origin and significance of a laminated aragonitic encrustation of Mediterranean supralittoral rocks Available to Purchase
ABSTRACT In this paper, we review ~140 yr of investigations about pelagosite, a usually black aragonitic encrustation with a vitreous luster that forms in the splash zone of Mediterranean rocky coasts. Prior to the mid-1920s, the geologic community considered pelagosite to be a separate mineral of uncertain composition, but then in 1926, Italian mineralogist Ettore Onorato determined that pelagosite has the same structure as aragonite (orthorhombic CaCO 3 ), and also that it contained cells of blue-green algae (i.e., cyanobacteria). Once pelagosite was declassed from the status of a mineral, and its name was eliminated from catalogues and textbooks, Onorato’s documentation of the cyanobacterial cells contained in this encrustation seems to have fallen into almost total oblivion during the rest of the twentieth century. We revisited pelagosite in its original type locality, the remote southern Adriatic island of Pelagosa (today’s Croatian island of Palagruža), as well as in the Dalmatian island of Hvar. Using modern analytical methods and techniques, we redefined the mineralogical and geochemical composition of pelagosite, the nature and significance of its microbial content, and the origin of its pisolitic “tree-ring” internal structure, which probably reflects cyclic climate changes.
Preliminary analysis of the decrease in water level of Vrana Lake on the small carbonate island of Cres (Dinaric karst, Croatia) Available to Purchase
Abstract A strong and potentially dangerous decreasing trend in the level of water in Vrana Lake over the last three decades was analysed. This freshwater lake is a unique karst hydrology feature located on the small Adriatic island of Cres (405.71 km 2 ), which is entirely composed of carbonate rocks. The lake is situated in a large cryptodepression and its base reaches a depth of 61.3 m below mean sea-level. The lake is a complex hydrological–hydrogeological system with an average water volume of c. 220 × 10 6 m 3 . The larger geographical region has been affected by an increase in air temperature over the last c. 40 years. This exceptionally clean freshwater lake is the only source of potable water for the whole Cres archipelago. A dangerous drop in the water level of the lake started in 1983. This decreasing trend is driven by both global climate change and anthropogenic (the overexploitation of water) factors.
Early Cretaceous tectonic event in the Adria: Insight from Umbria-Marche pelagic basin (Italy) Available to Purchase
Soft-sediment deformation structures crop out in the Lower Cretaceous succession of the Gubbio anticline in the Umbria-Marche Apennines of Italy. The deformation interval is ~13 m thick and occurs between the upper Hauterivian–lower Aptian Maiolica Formation and the Aptian Marne a Fucoidi Formation. It can be observed along the anticline for a distance of 12 km. Different types of deformation structures are distributed in several outcrops, with detachment extensional structures prevailing in the southeast sector. Imbricated slides, slump structures, and chaotic layers are distributed vertically and longitudinally in the middle and/or lower part of the deformed sediments. In the northwest sector of the anticline, compressional duplex structures can be considered the lower section of a large sediment failure. Geometrical and kinematic analysis of the fold axis trends and sliding surfaces have led to infer a single, large gravitational event possibly Albian in age. The synsedimentary deformation could be activated by several internal trigger mechanisms induced by external regional tectonic events such as earthquakes. An orthogonal system of calcite veins crossing the limestone layers represents the primary pathway for fluid-driven breaching of joint seals. These fluids can be related to the significant increase in the total organic carbon in the Hauterivian–Aptian layer of the Maiolica and Marne a Fucoidi Formations. This suggests the possibility that the limestone layer, sandwiched and sealed between clay of the organic-rich black shales, could have favored a pore pressure increase approaching lithostatic stress. With a thin overburden, lithostatic stress is more easily reached at low hydrostatic pressure. This slump sheet occurrence suggests the existence of a local paleoslope dipping toward the north-northwest, where the mass involved in the deformation is distributed over an estimated area of 60 km 2 for a volume of 0.8 km 3 of displaced sediments. The restoration and rotation of the slump fold hinges to the Early Cretaceous direction, in line with available paleomagnetic data, have shown that the strike of the slope corresponds to the main trend of the oldest Jurassic extensional lineaments and is linked to transform faults of the westernmost Tethys rifting systems.