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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Altiplano (41)
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Asia
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Far East
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Indonesia (1)
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Lesser Sunda Islands
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Malay Archipelago
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hydrogen
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D/H (3)
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Cs-137 (1)
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Pb-206/Pb-204 (9)
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Pb-207/Pb-204 (7)
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Pb-208/Pb-204 (7)
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Pb-210 (1)
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stable isotopes
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C-13/C-12 (2)
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D/H (3)
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Fe-56/Fe-54 (1)
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He-4/He-3 (1)
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Hf-177/Hf-176 (1)
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Nd-144/Nd-143 (11)
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O-17/O-16 (1)
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O-18/O-16 (7)
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Pb-206/Pb-204 (9)
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Pb-207/Pb-204 (7)
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Pb-208/Pb-204 (7)
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magnesium (1)
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hafnium
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iron
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trace metals (1)
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fossils
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Chordata
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Mammalia
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Theria
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Invertebrata
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Mollusca
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Protista
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Foraminifera (1)
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Plantae
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geochronology methods
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Paleogene
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Oligocene
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upper Cenozoic (6)
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Mesozoic
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middle Mesozoic (1)
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upper Mesozoic (1)
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Paleozoic
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Proterozoic (5)
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igneous rocks
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pyroclastics
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ring silicates
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clay minerals
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illite (1)
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sulfates
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-
-
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Primary terms
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absolute age (47)
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Asia
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Far East
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Indonesia (1)
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Lesser Sunda Islands
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Timor (1)
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Taiwan (1)
-
-
-
Atlantic Ocean
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South Atlantic
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Southwest Atlantic (1)
-
-
-
brines (5)
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carbon
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C-13/C-12 (2)
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C-14 (3)
-
-
Cenozoic
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Quaternary
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Holocene
-
lower Holocene (1)
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upper Holocene (1)
-
-
Pleistocene
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middle Pleistocene (1)
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upper Pleistocene (4)
-
-
-
Tertiary
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lower Tertiary (1)
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Neogene
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Miocene
-
lower Miocene (4)
-
middle Miocene (3)
-
upper Miocene (9)
-
-
Pliocene
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lower Pliocene (2)
-
-
-
Paleogene
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Eocene
-
middle Eocene (1)
-
upper Eocene (1)
-
-
Oligocene
-
lower Oligocene (1)
-
upper Oligocene (2)
-
-
Paleocene
-
lower Paleocene (2)
-
-
-
-
upper Cenozoic (6)
-
-
Central America (2)
-
ceramic materials (1)
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Chordata
-
Vertebrata
-
Tetrapoda
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Mammalia
-
Theria
-
Eutheria
-
Notoungulata (2)
-
-
-
-
-
-
-
clay mineralogy (1)
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climate change (9)
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construction materials (1)
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crust (45)
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data processing (7)
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deformation (30)
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diagenesis (2)
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earthquakes (4)
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ecology (1)
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epeirogeny (1)
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Europe
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Alps
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Eastern Alps (1)
-
-
Southern Europe
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Italy
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Apennines
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Central Apennines (1)
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-
-
-
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evaporite deposits (2)
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faults (38)
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foliation (2)
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foundations (1)
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geochemistry (28)
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geomorphology (17)
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geophysical methods (15)
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hydrogen
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D/H (3)
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tritium (1)
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hydrology (2)
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ichnofossils (1)
-
igneous rocks
-
plutonic rocks
-
diorites
-
tonalite (1)
-
-
granites
-
A-type granites (1)
-
I-type granites (1)
-
monzogranite (2)
-
S-type granites (2)
-
-
granodiorites (3)
-
ultramafics
-
peridotites (1)
-
pyroxenite (1)
-
-
-
porphyry (1)
-
volcanic rocks
-
andesites (9)
-
basalts
-
flood basalts (1)
-
mid-ocean ridge basalts (2)
-
shoshonite (1)
-
-
dacites (3)
-
glasses
-
volcanic glass (4)
-
-
pyroclastics
-
ignimbrite (15)
-
pumice (3)
-
tuff (3)
-
-
rhyodacites (1)
-
rhyolites (4)
-
trachyandesites (1)
-
-
-
inclusions
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fluid inclusions (6)
-
-
industrial minerals (1)
-
intrusions (25)
-
Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Ostracoda (1)
-
-
-
-
Mollusca
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Bivalvia (1)
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Cephalopoda
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Ammonoidea (1)
-
-
Gastropoda (1)
-
-
Protista
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Foraminifera (1)
-
-
-
isostasy (2)
-
isotopes
-
radioactive isotopes
-
Be-10 (2)
-
C-14 (3)
-
Cs-137 (1)
-
Pb-206/Pb-204 (9)
-
Pb-207/Pb-204 (7)
-
Pb-208/Pb-204 (7)
-
Pb-210 (1)
-
tritium (1)
-
-
stable isotopes
-
C-13/C-12 (2)
-
D/H (3)
-
Fe-56/Fe-54 (1)
-
He-4/He-3 (1)
-
Hf-177/Hf-176 (1)
-
Nd-144/Nd-143 (11)
-
O-17/O-16 (1)
-
O-18/O-16 (7)
-
Pb-206/Pb-204 (9)
-
Pb-207/Pb-204 (7)
-
Pb-208/Pb-204 (7)
-
S-34/S-32 (2)
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Sr-87/Sr-86 (16)
-
-
-
land use (1)
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lava (11)
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lineation (1)
-
magmas (29)
-
Malay Archipelago
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Timor (1)
-
-
mantle (11)
-
Mesozoic
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Cretaceous
-
Lower Cretaceous
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Agrio Formation (1)
-
-
Middle Cretaceous (2)
-
Upper Cretaceous
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Maestrichtian (1)
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Turonian (1)
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-
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Jurassic
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Lower Jurassic (1)
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Middle Jurassic (2)
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Upper Jurassic (2)
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middle Mesozoic (1)
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Triassic
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Lower Triassic (2)
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Middle Triassic (1)
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upper Mesozoic (1)
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Vaca Muerta Formation (1)
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metal ores
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antimony ores (1)
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base metals (3)
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bismuth ores (1)
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copper ores (21)
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gold ores (9)
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IOCG deposits (2)
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iron ores (2)
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lead ores (3)
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lead-zinc deposits (2)
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manganese ores (1)
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molybdenum ores (8)
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polymetallic ores (4)
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silver ores (6)
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tin ores (9)
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tungsten ores (2)
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zinc ores (2)
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metals
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alkali metals
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cesium
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Cs-137 (1)
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rubidium (1)
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alkaline earth metals
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barium (1)
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beryllium
-
Be-10 (2)
-
-
magnesium (1)
-
strontium
-
Sr-87/Sr-86 (16)
-
-
-
hafnium
-
Hf-177/Hf-176 (1)
-
-
iron
-
Fe-56/Fe-54 (1)
-
-
lead
-
Pb-206/Pb-204 (9)
-
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Central Andes
Controls of the Lithospheric Thermal Field of an Ocean-Continent Subduction Zone: The Southern Central Andes
Kinematic evolution of the central Andean retroarc thrust belt in northwestern Argentina and implications for coupling between shortening and crustal thickening
Emplacement conditions and exhumation of the Varvarco Tonalite and associated plutons from the Cordillera del Viento, Southern Central Andes
What drives Fe depletion in calc-alkaline magma differentiation: Insights from Fe isotopes
Tectonic and paleoclimatic controls on the composition of inland wetland deposits, Chaco foreland basin, Central Andes
Detrital zircon record of Phanerozoic magmatism in the southern Central Andes
ABSTRACT Uplift of the central Andes during the Miocene was followed by large-scale reorganization of Atlantic-draining rivers in Argentine Patagonia. Here, we document the abandonment of one large river in the late Pliocene and the establishment of the modern drainage in the Early Pleistocene. A chronology for these events is provided by 40 Ar/ 39 Ar ages on basalt flows. Remnants of the Pliocene paleovalley system are well preserved in the Lago Cardiel–Gobernador Gregores area, where they are eroded into flat-lying basalt flows dated from ca. 13.9 Ma to 8.6 Ma. Younger basalts that erupted onto the abandoned floor of the paleovalley are as young as 3.7 Ma. Abandonment of the Pliocene paleovalley and establishment of the modern Río Chico and Río Shehuen catchments happened near the close of the Pliocene when Andean glaciers incised the east-sloping pediment on which the late Miocene drainage was established. Lago Cardiel sits within a large endorheic basin that is inset into the late Pliocene paleovalley. The basin began to develop just before 4 Ma, after the paleovalley was abandoned. It became larger and deeper during the Pleistocene due to mass movements along its margins, deflation of the basin floor during times when Lago Cardiel was dry or nearly dry, and possibly lowering along bounding faults. The Pliocene–Pleistocene landscape and drainage changes that we have documented are not unique to the Lago Cardiel–Gobernador Gregores area; similar changes are apparent elsewhere in Patagonia east of the crest of the Andes.
Lithospheric Structure of the Central Andes Forearc from Gravity Data Modeling: Implication for Plate Coupling
Case Study: Reconstructing the 2015 Dulcepamba River Flood Disaster
Geological development of the Timor Orogen
Abstract The Timor Orogen comprises the island of Timor, a narrow offshore area to the north and a wider offshore fold-and-thrust belt to the south. This orogen formed by jamming and subsequent collision of the Banda Sea subduction system by the Australian Plate. The BandaSeis seismic survey has revealed excellent images of the deep-water fold-and-thrust belt. Seismic interpretation of the dataset demonstrated structural and tectonic features not previously described, including regional geological features on the Australian continental crust and two regional NE–SW sinistral strike-slip faults, and a prominent Middle Permian palaeogeographical high (Timor Plateau). Moreover, since the Middle–Late Triassic and Middle Jurassic, the two NE-trending strike-slip faults governed the formation of the West Timor and Cova-Lima sub-basins. The location along the Australian margin plays a dominant role in controlling the structural style and shaping of the Timor Orogen. Vertical loading and the southerly motion of the orogenic wedge are the main driving forces responsible for its building, illustrating a thin-skinned tectonic framework. Thrust faults nucleate in a forward-breaking sequence in the motion of thrust transport, with younger thrusts developing in front of older thrusts. Most of the collisional deformation has been classified into two styles: shallow thin-skinned and deep-seated deformation.