- 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
-
Asia
-
Far East
-
Borneo
-
Kalimantan Indonesia (5)
-
-
Indonesia
-
Bali (1)
-
Celebes (1)
-
Java (5)
-
Kalimantan Indonesia (5)
-
Sumatra (4)
-
Sunda Arc (1)
-
-
Lesser Sunda Islands
-
Bali (1)
-
-
Malay Peninsula (1)
-
-
Southeast Asia (3)
-
Strait of Malacca (1)
-
-
Caribbean region
-
West Indies
-
Antilles
-
Lesser Antilles
-
Barbados (1)
-
-
-
-
-
Indian Ocean
-
Andaman Sea (1)
-
Timor Sea
-
Sahul Shelf (1)
-
-
-
Kutei Basin (1)
-
Malay Archipelago
-
Borneo
-
Kalimantan Indonesia (5)
-
-
-
North America
-
Appalachian Basin (1)
-
-
Pacific Ocean
-
North Pacific
-
Northwest Pacific
-
Celebes Sea (1)
-
South China Sea (3)
-
-
-
Pacific Basin (1)
-
South Pacific
-
Southwest Pacific
-
Java Sea (25)
-
-
-
West Pacific
-
Indonesian Seas
-
Celebes Sea (1)
-
Java Sea (25)
-
-
Northwest Pacific
-
Celebes Sea (1)
-
South China Sea (3)
-
-
Southwest Pacific
-
Java Sea (25)
-
-
Sunda Shelf (11)
-
-
-
South America (1)
-
-
commodities
-
oil and gas fields (4)
-
petroleum
-
natural gas (4)
-
-
-
elements, isotopes
-
carbon
-
C-13/C-12 (1)
-
C-14 (1)
-
-
isotope ratios (1)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
-
stable isotopes
-
C-13/C-12 (1)
-
N-15/N-14 (1)
-
-
-
nitrogen
-
N-15/N-14 (1)
-
-
-
fossils
-
borings (1)
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Primates
-
Hominidae
-
Homo (1)
-
-
-
-
-
-
-
-
-
Invertebrata
-
Cnidaria
-
Anthozoa
-
Zoantharia
-
Scleractinia
-
Acropora
-
Acropora palmata (1)
-
-
-
-
-
-
Mollusca (1)
-
Protista
-
Foraminifera
-
Rotaliina
-
Rotaliacea
-
Heterostegina
-
Heterostegina depressa (1)
-
-
-
-
-
-
-
microfossils (3)
-
palynomorphs
-
Dinoflagellata (1)
-
-
Plantae
-
algae
-
Chlorophyta
-
Chlorophyceae
-
Codiaceae
-
Halimeda (1)
-
-
-
-
nannofossils (1)
-
-
-
thallophytes (1)
-
-
geochronology methods
-
U/Pb (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Holocene
-
upper Holocene (1)
-
-
Pleistocene (3)
-
-
Tertiary
-
Neogene
-
Miocene (2)
-
Pliocene (1)
-
-
Paleogene (1)
-
-
upper Cenozoic (1)
-
-
Mesozoic
-
Cretaceous (1)
-
-
Paleozoic
-
Carboniferous
-
Pennsylvanian (1)
-
-
upper Paleozoic (1)
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks (1)
-
-
ophiolite (1)
-
-
metamorphic rocks
-
ophiolite (1)
-
-
minerals
-
silicates
-
framework silicates
-
feldspar group
-
alkali feldspar
-
orthoclase (1)
-
-
plagioclase (1)
-
-
silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
sheet silicates
-
clay minerals
-
kaolinite (1)
-
montmorillonite (1)
-
-
illite (1)
-
-
-
-
Primary terms
-
absolute age (2)
-
Asia
-
Far East
-
Borneo
-
Kalimantan Indonesia (5)
-
-
Indonesia
-
Bali (1)
-
Celebes (1)
-
Java (5)
-
Kalimantan Indonesia (5)
-
Sumatra (4)
-
Sunda Arc (1)
-
-
Lesser Sunda Islands
-
Bali (1)
-
-
Malay Peninsula (1)
-
-
Southeast Asia (3)
-
Strait of Malacca (1)
-
-
biogeography (1)
-
carbon
-
C-13/C-12 (1)
-
C-14 (1)
-
-
Caribbean region
-
West Indies
-
Antilles
-
Lesser Antilles
-
Barbados (1)
-
-
-
-
-
Cenozoic
-
Quaternary
-
Holocene
-
upper Holocene (1)
-
-
Pleistocene (3)
-
-
Tertiary
-
Neogene
-
Miocene (2)
-
Pliocene (1)
-
-
Paleogene (1)
-
-
upper Cenozoic (1)
-
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Primates
-
Hominidae
-
Homo (1)
-
-
-
-
-
-
-
-
-
climate change (2)
-
continental shelf (2)
-
ecology (1)
-
economic geology (1)
-
faults (2)
-
geophysical methods (9)
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks (1)
-
-
Indian Ocean
-
Andaman Sea (1)
-
Timor Sea
-
Sahul Shelf (1)
-
-
-
Invertebrata
-
Cnidaria
-
Anthozoa
-
Zoantharia
-
Scleractinia
-
Acropora
-
Acropora palmata (1)
-
-
-
-
-
-
Mollusca (1)
-
Protista
-
Foraminifera
-
Rotaliina
-
Rotaliacea
-
Heterostegina
-
Heterostegina depressa (1)
-
-
-
-
-
-
-
isostasy (1)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
-
stable isotopes
-
C-13/C-12 (1)
-
N-15/N-14 (1)
-
-
-
Malay Archipelago
-
Borneo
-
Kalimantan Indonesia (5)
-
-
-
mantle (1)
-
Mesozoic
-
Cretaceous (1)
-
-
nitrogen
-
N-15/N-14 (1)
-
-
North America
-
Appalachian Basin (1)
-
-
ocean floors (3)
-
oceanography (4)
-
oil and gas fields (4)
-
Pacific Ocean
-
North Pacific
-
Northwest Pacific
-
Celebes Sea (1)
-
South China Sea (3)
-
-
-
Pacific Basin (1)
-
South Pacific
-
Southwest Pacific
-
Java Sea (25)
-
-
-
West Pacific
-
Indonesian Seas
-
Celebes Sea (1)
-
Java Sea (25)
-
-
Northwest Pacific
-
Celebes Sea (1)
-
South China Sea (3)
-
-
Southwest Pacific
-
Java Sea (25)
-
-
Sunda Shelf (11)
-
-
-
paleogeography (5)
-
paleontology (2)
-
Paleozoic
-
Carboniferous
-
Pennsylvanian (1)
-
-
upper Paleozoic (1)
-
-
palynomorphs
-
Dinoflagellata (1)
-
-
petroleum
-
natural gas (4)
-
-
petrology (1)
-
Plantae
-
algae
-
Chlorophyta
-
Chlorophyceae
-
Codiaceae
-
Halimeda (1)
-
-
-
-
nannofossils (1)
-
-
-
plate tectonics (4)
-
reefs (1)
-
sea-level changes (7)
-
sedimentary petrology (1)
-
sedimentary rocks
-
carbonate rocks
-
boundstone (1)
-
limestone (2)
-
packstone (1)
-
wackestone (1)
-
-
clastic rocks
-
arenite
-
quartz arenite (1)
-
-
sandstone (4)
-
-
coal (1)
-
gas sands (1)
-
-
sedimentary structures
-
biogenic structures
-
algal structures
-
algal mounds (1)
-
-
bioherms (1)
-
carbonate banks (1)
-
-
-
sedimentation (5)
-
sediments
-
marine sediments (4)
-
peat (1)
-
-
shorelines (1)
-
South America (1)
-
stratigraphy (4)
-
structural geology (1)
-
tectonics (2)
-
tectonophysics (1)
-
thallophytes (1)
-
well-logging (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
boundstone (1)
-
limestone (2)
-
packstone (1)
-
wackestone (1)
-
-
clastic rocks
-
arenite
-
quartz arenite (1)
-
-
sandstone (4)
-
-
coal (1)
-
gas sands (1)
-
-
siliciclastics (1)
-
-
sedimentary structures
-
borings (1)
-
sedimentary structures
-
biogenic structures
-
algal structures
-
algal mounds (1)
-
-
bioherms (1)
-
carbonate banks (1)
-
-
-
-
sediments
-
sediments
-
marine sediments (4)
-
peat (1)
-
-
siliciclastics (1)
-
Java Sea
High-resolution multi-proxy reconstruction of environmental changes in coastal waters of the Java Sea, Indonesia, during the late Holocene
Abstract Past environments of equatorial SE Asia must have played a critical role in determining the timing and trajectory of early human dispersal into and through the region. However, very few reliable terrestrial records are available with which to contextualize human dispersal events. This circumstance, coupled with a sparse archaeological record and the likelihood that much of the archaeological record is now submerged, means we have an incomplete understanding of the role that geography, climate and environment played in shaping human pre-history in this region. From a review of the literature, we conclude that there must have been a substantial environmental barrier resulting in a genetic separation between east and west Sundaland that persisted even though a terrestrial connection was present for most of the Pleistocene. This barrier is likely to be a north–south corridor of open non-forest vegetation, and its existence may have encouraged the rapid dispersal of early humans through the interior of Sundaland and on to Sahul. We conclude that more reliable terrestrial palaeoenvironmental records are required to better understand the links between past environments and dispersal events. We highlight avenues of particular research value, such as focusing on eastern Sumatra, western/southern Borneo and the islands in the Java Sea, where the purported savanna corridor most probably existed, and including edaphic factors in palaeovegetation modelling.
BENTHIC FORAMINIFERA IN A LARGE INDO-PACIFIC CORAL REEF AQUARIUM
The stratigraphic record of volcanic arcs provides insights into their eruptive history, the formation of associated basins, and the character of the deep crust beneath them. Indian Ocean lithosphere was subducted continuously beneath Java from ca. 45 Ma, resulting in formation of a volcanic arc, although volcanic activity was not continuous for all of this period. The lower Cenozoic stratigraphic record on land in East Java provides an excellent opportunity to examine the complete eruptive history of a young, well-preserved volcanic arc from initiation to termination. The Southern Mountains Arc in Java was active from the middle Eocene (ca. 45 Ma) to the early Miocene (ca. 20 Ma), and its activity included significant acidic volcanism that was overlooked in previous studies of the area. In particular, quartz sandstones, previously considered to be terrigenous clastic sedimentary rocks derived from continental crust, are now known to be of volcanic origin. These deposits form part of the fill of the Kendeng Basin, a deep flexural basin that formed in the backarc area, north of the arc. Dating of zircons in the arc rocks indicates that the acidic character of the volcanism can be related to contamination of magmas by a fragment of Archean to Cambrian continental crust that lay beneath the arc. Activity in the Southern Mountains Arc ended in the early Miocene (ca. 20 Ma) with a phase of intense eruptions, including the Semilir event, which distributed ash over a wide area. Following the cessation of the early Cenozoic arc volcanism, there followed a period of volcanic quiescence. Subsequently arc volcanism resumed in the late Miocene (ca. 12–10 Ma) in the modern Sunda Arc, the axis of which lies 50 km north of the older arc.
Three-Dimensional Seismic Architecture of Fluvial Sequences on the Low-Gradient Sunda Shelf, Offshore Indonesia
Postglacial coastal evolution: Ice–ocean–solid Earth interactions in a period of rapid climate change
The most recent glacial-interglacial transition of the late Pleistocene ice age was accompanied by an increase in globally averaged ice-equivalent eustatic sea level of ∼120 m. This increase in sea level occurred over a period of ∼10,000 yr and was accompanied by highly significant regional inundations of the land by the sea as well as by significant regional emergence of the land from the sea in the initially ice-covered regions. These migrations of the coastline can be accurately predicted given only an assumed known history of the deglaciation of the continents. An especially interesting aspect of the suite of physical interactions involved in the global process of glacial isostatic adjustment concerns the influence of variations in the Earth's rotation on the local histories of relative sea level, which may be inferred on the basis of radiocarbon dating of suitable sea-level index points. The observed variability in sea level may be interpreted in terms of fundamentally important climatological and solid Earth geophysical properties of Earth System processes that govern system evolution.
Linked lowstand delta to basin-floor fan deposition, offshore Indonesia: An analog for deep-water reservoir systems
3-D seismic geomorphology: Insights into fluvial reservoir deposition and performance, Widuri field, Java Sea
Mollusc Shell Encrustation and Bioerosion Rates in a Modern Epeiric Sea: Taphonomy Experiments in the Java Sea, Indonesia
Ancient Shelf Ridges—A Potentially Significant Component of the Transgressive Systems Tract: Case Study from Offshore Northwest Java
Lowstand Alluvial Bypass Systems: Incised vs. Unincised
3-D seismic interpretation of thin gas sandstone reservoirs using multiattribute analysis on poststack and AVO data, offshore SE Sumatra
Tomographic and geological constraints on subduction along the eastern Sundaland continental margin (South-East Asia)
Recent sedimentation patterns in the central Sumatra basin, Republic of Indonesia, may help to explain the cyclic stratigraphy of the Pennsylvanian System of the eastern United States. Modern influx of fluvial siliciclastic sediment to the epeiric seas of the Sunda shelf, including the Strait of Malacca, appears to be highly restricted by rain forest cover within the ever-wet climate belt of equatorial Sumatra. As a result, much of the marine and estuarine environments appear to be erosional or nondepositional except for localized deposition of sediment in slack water areas, such as the down-stream end of islands. Contemporaneously, thick (>13 m), laterally extensive (>70,000 km 2 ), peat deposits are forming on poorly drained coastal lowlands. Modern peat formation in this study, therefore, is not coeval with aggrading fluvial siliciclastic systems, a situation that commonly is assumed in many depositional models of coal formation. The stratigraphy of Pleistocene and Holocene sediments on the Sunda shelf, as well as those of the Pennsylvanian System, appears to be better explained by the allocyclic controls of climate and sea-level change on sediment flux rather than by depositional models that are based on autocyclic processes. The objective of this paper is to evaluate allocyclic and autocyclic controls on sedimentation in an epeiric setting in a humid (ever-wet) tropical region. Of particular interest are the factors that control peat formation and siliciclastic sediment flux in rivers, estuaries, and open marine environments.