Petrogenesis of diachronous mixed siliciclastic‐carbonate megafacies in the cool‐water Oligocene Tikorangi formation, Taranaki Basin, New Zealand
نویسندگان
چکیده
منابع مشابه
Fault Visualization Enhancement Using Ant Tracking Technique and Its Application in the Taranaki Basin, New Zealand
The ant tracking technique has been widely used in fault interpretation. However, the reliability of the results is highly dependent on appropriately choosing signal processing method and volume attributes. In our study area, which lies in the southern Taranaki Basin, we applied Graphic Equalizer as the processing tool and the Chaos attribute before running the ant tracking algorithm. Results s...
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Pollen and charcoal analyses of sediments from northern coastal Taranaki, New Zealand, show that Maori settlement impacts on the vegetation began with the burning of tall coastal forest in the mid-17th century. Forest was replaced with a fern-shrubland, and small wetlands expanded with changing hydrological conditions. This forest clearance was much later than in most regions of the country, wh...
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The early-mid Paleocene Farewell Formation is stratigraphically distributed across the 10 southern Taranaki Basin (STB) which is also encountered within the Maui Gas Field. Using 11 available 3D seismic and well log data, a challenging task to delineate the spatial distribution and 12 geobody patterns of the potential reservoir sands of the formation was performed. Object based 13 modeling coup...
متن کاملSealers Bay submarine fan complex, Oligocene, southern New Zealand
The Oligocene Balleny Group of Chalky Island, southwestern Fiordland, comprises a typical continental margin sequence 900 m in thickness. Thin nearshore traction deposited sediments at the base are overlain by submarine canyon and fan lithofacies that were deposited by the full range of subaqueous mass-transport processes. A steep-walled channel within Balleny Group is interpreted as a fossil p...
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ژورنال
عنوان ژورنال: New Zealand Journal of Geology and Geophysics
سال: 2003
ISSN: 0028-8306,1175-8791
DOI: 10.1080/00288306.2003.9515016