- 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
-
Africa
-
Southern Africa
-
South Africa
-
KwaZulu-Natal South Africa
-
Zululand (1)
-
-
-
-
-
Australasia
-
Australia
-
Great Artesian Basin (16)
-
New South Wales Australia (2)
-
Queensland Australia (5)
-
South Australia
-
Kangaroo Island (1)
-
-
Tasmania Australia (1)
-
Victoria Australia (1)
-
Western Australia (1)
-
-
Papua New Guinea (1)
-
-
Eucla Basin (1)
-
Murray Basin (2)
-
Southern Hemisphere (1)
-
Sydney Basin (1)
-
-
commodities
-
bitumens (1)
-
gems (1)
-
oil and gas fields (1)
-
petroleum
-
natural gas (1)
-
-
-
elements, isotopes
-
isotopes
-
stable isotopes
-
Sr-87/Sr-86 (1)
-
-
-
metals
-
alkaline earth metals
-
calcium (1)
-
strontium
-
Sr-87/Sr-86 (1)
-
-
-
-
-
fossils
-
Invertebrata
-
Mollusca
-
Cephalopoda
-
Ammonoidea (1)
-
-
-
Protista
-
Foraminifera
-
Rotaliina
-
Orbitoidacea
-
Lepidocyclina (1)
-
-
Rotaliacea
-
Nummulitidae
-
Nummulites (1)
-
-
-
-
Textulariina
-
Lituolacea
-
Orbitolinidae
-
Orbitolina (1)
-
-
-
-
-
-
-
microfossils (5)
-
-
geologic age
-
Cenozoic
-
Tertiary (1)
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (3)
-
-
Toolebuc Formation (1)
-
Upper Cretaceous
-
Cenomanian (2)
-
-
-
Jurassic (2)
-
-
Paleozoic
-
Permian (1)
-
-
-
minerals
-
silicates
-
framework silicates
-
silica minerals
-
opal
-
opal-A (1)
-
-
-
-
-
-
Primary terms
-
Africa
-
Southern Africa
-
South Africa
-
KwaZulu-Natal South Africa
-
Zululand (1)
-
-
-
-
-
Australasia
-
Australia
-
Great Artesian Basin (16)
-
New South Wales Australia (2)
-
Queensland Australia (5)
-
South Australia
-
Kangaroo Island (1)
-
-
Tasmania Australia (1)
-
Victoria Australia (1)
-
Western Australia (1)
-
-
Papua New Guinea (1)
-
-
bitumens (1)
-
Cenozoic
-
Tertiary (1)
-
-
continental drift (1)
-
diagenesis (1)
-
economic geology (2)
-
gems (1)
-
geochemistry (1)
-
geomorphology (1)
-
government agencies (1)
-
ground water (3)
-
hydrogeology (1)
-
Invertebrata
-
Mollusca
-
Cephalopoda
-
Ammonoidea (1)
-
-
-
Protista
-
Foraminifera
-
Rotaliina
-
Orbitoidacea
-
Lepidocyclina (1)
-
-
Rotaliacea
-
Nummulitidae
-
Nummulites (1)
-
-
-
-
Textulariina
-
Lituolacea
-
Orbitolinidae
-
Orbitolina (1)
-
-
-
-
-
-
-
isotopes
-
stable isotopes
-
Sr-87/Sr-86 (1)
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (3)
-
-
Toolebuc Formation (1)
-
Upper Cretaceous
-
Cenomanian (2)
-
-
-
Jurassic (2)
-
-
metals
-
alkaline earth metals
-
calcium (1)
-
strontium
-
Sr-87/Sr-86 (1)
-
-
-
-
oil and gas fields (1)
-
paleoecology (2)
-
paleogeography (2)
-
paleontology (3)
-
Paleozoic
-
Permian (1)
-
-
petroleum
-
natural gas (1)
-
-
sedimentary rocks
-
carbonate rocks
-
limestone
-
microbialite (1)
-
-
travertine (1)
-
-
chemically precipitated rocks
-
tufa (1)
-
-
coal (1)
-
oil shale (1)
-
-
sedimentation (1)
-
Southern Hemisphere (1)
-
springs (1)
-
stratigraphy (4)
-
structural geology (1)
-
tectonics (1)
-
thermal waters (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
limestone
-
microbialite (1)
-
-
travertine (1)
-
-
chemically precipitated rocks
-
tufa (1)
-
-
coal (1)
-
oil shale (1)
-
-
Great Artesian Basin
Ground waters with unradiogenic 87 Sr/ 86 Sr ratios in the Great Artesian Basin, Australia
Albian foraminifera of Zululand (South Africa) and Great Artesian Basin (Australia)
Some interesting foraminifera from the Cretaceous of the Great Artesian Basin, Australia
Bilingulogavelinella australis n. gen. n. sp (foraminifera) from the marine Cretaceous of the Great Artesian Basin, Australia
Lingulogavelinella (Foraminifera) in the Cretaceous of the Great Artesian Basin, Australia
Basal Jurassic-Cretaceous Rocks of Western Great Artesian Basin, South Australia: Stratigraphy and Environment
Australia, Geophysical Exploration, and Great Artesian Basin: ABSTRACT
Distribution of Paleozoic Rocks Beneath Great Artesian Basin, Queensland
Petroleum Prospects of Western Parts of Great Australian Artesian Basin
Australian sedimentary opal-A and its associated minerals: Implications for natural silica sphere formation
Groundwater head in high-temperature aquifers
Foraminifers and Continental Drift
A Review of the Oil and Gas Prospects of Australia
Travertine and tufa from Dalhousie Springs (Australia)—Implications for recognizing Martian springs
Thermal spring deposits are features of considerable interest to Mars scientists because of their potential as astrobiological oases and as records of the paleohydrology of the planet. Terrestrial counterparts can assist in recognizing such features on Mars and in developing technologies for their study and sampling. In this paper, we describe one such analog, the Dalhousie Springs complex in central Australia. The Dalhousie Springs complex is one of largest groundwater discharge landforms known on Earth. It is a carbonate-limited precipitation system due to the non-supersaturated ascending water. Spring carbonates are deposited as discrete mounds and outflow channels resting unconformably on older units. Although subject to postformation geomorphic modification, the spring deposits persist in the landscape and are recognizable long after the parental spring has shut down. We identify 14 specific microfacies belonging to seven facies, which form three environmental associations related to specific depositional environments. Diagenesis has occurred in several stages, as evidenced by distinctive textures on the deposits. Spring deposits on Mars would potentially be recognized by similar textures (although compositions may be quite different) and similar geomorphic relationships. However, in satellite images, spring deposits may be difficult to differentiate from deposits resulting from other processes that produce similar geomorphic features, including mud volcanoes, pingos, and rootless cones. Mineralogical data may assist, but ultimately ground truth will be required.