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1.
Chris Klootwijk John Giddings Chris Pigram Charles Loxton Hugh Davies Rick Rogerson David Falvey 《Tectonophysics》2003,362(1-4):239-272
Oblique convergence since the Early Cenozoic between the northward-moving Australian plate, westward-moving Pacific plate and almost stationary Eurasian plate has created a world-ranking tectonic zone in the eastern Indonesia–New Guinea–Southwest Pacific region (Tonga–Sulawesi megashear) that is notorious for its complex mix of tectonic styles and terrane juxtapositions. Unlike an ancient analog—the Mesozoic–Cenozoic Cordillera of North America—palaeomagnetic constraints on terrane motions in the zone are few. To improve the framework of quantitative control on such motions and therefore our understanding of the development of the zone, results of a palaeomagnetic study in the Highlands region of Papua New Guinea (PNG), in the southern part of the New Guinea Orogen, are reported. The study yields new insights into terrane tectonics along the Australian craton's active northern margin and confirms the complexity of block rotations to be expected at the local scale in tectonically intricate zones. The study is based on more than 500 samples (21 localities) collected from an interior and an exterior zone of New Guinea's central cordillera. The two zones are separated by the Tahin and Stolle–Lagaip–Kaugel Fault zones and collectively represent the para-autochthonous northern margin of the Australian craton. Samples from the interior zone, which in the study area comprises a cratonic spur of uncertain—probably displaced—origin, come from Triassic to Miocene sediments and subordinate volcanics of the Kubor Anticline, Jimi Terrane, and Yaveufa Syncline (16 localities) in the central and eastern Highlands. Samples from the exterior zone, which represent a basement-involved, Pliocene foreland fold-and-thrust belt, come from Middle Eocene to Middle Miocene carbonates and clastics (five localities) in the southern Highlands of the Papuan Fold Belt. Results permit us to constrain the tectonic evolution of the two zones palaeomagnetically. Using mainly thermal demagnetization techniques, three main magnetic components have been identified in the collection: (1) a recent field overprint of both normal and reverse polarity; (2) a pervasive overprint of mainly normal polarity that originated during extensive Middle to Late Miocene intrusive activity in the central cordillera; and (3) a primary component which has been identified in only 7 of the 21 localities (5 of 11 stratigraphic units represented in the collection). All components show patterns of rotation that are consistent within the zones, but differ between them. In the interior zone (central and eastern Highlands), large-scale counterclockwise rotations of between 30°+ and 100°+ have been established throughout the Kubor Anticline and Jimi Terrane, with some clockwise rotation present in the southern part of the Yaveufa Syncline. In contrast, in the Mendi area of the exterior zone (southern Highlands), clockwise rotations of between 30°+ and 50°+ can be recognized. These contrasting rotation patterns across the Tahin and Stolle–Lagaip–Kaugel Fault zones indicate decoupling of the two tectonic zones, probably along basement-involved faults. The clockwise rotations in the southern Highlands of the Papuan Fold Belt are to be expected from its structural grain, and are probably governed by regional basement faults and transverse lineaments. In contrast, the pattern of counterclockwise rotations in the Kubor Anticline–Jimi Terrane cratonic spur of the central and eastern Highlands was unexpected. The pattern is interpreted to result from non-rigid rotation of continental terranes as they were transported westward across the northeastern margin of the Australian craton. This margin became reorganised after the Middle Miocene, when the steadily northward-advancing Australian craton impinged into the westward-moving Pacific plate/buffer-plate system. Transpressional reorganisation under the influence of the sinistral Tonga–Sulawesi megashear became enhanced with Mio-Pliocene docking, and subsequent southward overthrusting, of the Finisterre Terrane onto the northeastern margin of the Australian craton. 相似文献
2.
Giddings John W. Klootwijk Chris Rees John Groenewoud Adrian 《Geologie en Mijnbouw》1997,76(1-2):35-44
Since the early sixties, alternating field demagnetization (AFD) has been a standard laboratory technique for demagnetizing rocks to expose the multicomponent structure of their natural remanent magnetization (NRM). In the majority of AFD implementations, however, the procedure remains as labour-intensive as ever. The implementation that we have developed at the Australian Geological Survey Organisation, automates the procedure for AFD based on the static method, and results in significant productivity and efficiency gains without compromising data quality. A properly formulated procedure for static AFD may be the only method of retrieving higher-coercivity components of natural remanence in samples prone to developing gyroremanence at higher alternating fields (AFs). Our AFD environment comprises: a 2G-Enterprises through-bore, cryogenic magnetometer; 2G AF-coils and control equipment; and personal computer software, developed by us, to control all procedural aspects for a complete AFD of a sample including, importantly, a counteracting procedure to neutralize the effects of gyroremanence build-up at higher AFs. With our system, AFD of 8 samples/day, each of 20+ steps, requires only 20 min of user attention compared with a full day for conventional systems. 相似文献
3.
J.W. Giddings 《Tectonophysics》1976,30(1-2)
The palaeomagnetism of 54 dykes sampled from the many swarms that intrude the Yilgarn Block of Western Australia shows that their directions of magnetization fall into five distinct groups.Preliminary Rb-Sr age determinations made on samples used in the study however, indicate that for one, and possibly two of those groups, the dykes belong to two widely different ages suggesting that the palaeomagnetic field has been sampled at two widely separated points in time but when its direction was essentially the same. The seven groups of directions thus obtained imply that the dykes belong to at least six, possibly seven periods of intrusion. Relative-age information relating to four of those periods, determined from cross-cutting and baked contact studies, agrees with that obtained radiometrically.The poles and ages of the groups are as follows: Group YA dykes (c. 2500 or c. 1700 m.y.) 21.7S 133.7E (A95 = 17.9°) Group YB dykes (750—700 m.y.) 19.9S 282.0E (A95 = 28.1°) Group YC dykes (1500 m.y., Group YB) 79.7N 2.7E (A95 = 13.0°) Group YD dykes (1700 m.y.) 23.5S 46.1E (A95 = 9.9°) Group YE dykes (c. 2500 m.y.) 28.3S 0.4E (A95 = 31.0°) Group YF dykes (c. 1700 m.y.) 24.7N 101.8E (A95 = 14.0°) Ravensthorpe dykes (2500 ± 100 m.y.) 38.3S 136.2E (A95 = 25.5°)Results from eight samples of the 1390 ± 140 m.y. Morawa Lavas of the Billeranga Hills yield a pole at 42.8N 22.4E (A95 = 14.7°). 相似文献
4.
Late Precambrian and Lower Palaeozoic palaeomagnetic results from South Australia and Western Australia 总被引：1，自引：0，他引：1
Seismic reflection and refraction data are described from four locations in the eastern Mediterranean. Over the Mediterranean Ridge the profiles reveal a great thickness of material in the velocity range 3.6 – 5.5 km/sec. The crust is very disturbed and so penetration is limited, but at the foot of the Nile Cone an unreversed line gives a depth to the mantle of 27 km. This suggests that the crust in the eastern Mediterranean is more likely to be continental than oceanic in structure. 相似文献
5.
An examination of the deeply incised Ediacaran Wonoka canyons in the Adelaide Geosyncline (most recently interpreted as subaerial valleys) demonstrates their submarine origin, and confirms them as some of the best examples of ancient outcropping submarine canyons in the world. The entire canyon-fill succession is interpreted to be of deep-water (below wave base) origin, consisting of calcareous shale and siltstone together with a variety of mass-flow deposits including turbidites, grain flows and debris flows. The canyon fill lacks definitive shallow-water structures (e.g. mud cracks, fenestral fabrics or wave ripples) at all stratigraphic levels. Canyon-lining carbonate crusts that have previously been interpreted as non-marine calcretes or tufas (and used to suggest a non-marine origin for the canyons) are argued to be of deep-water, marine, microbial origin. Extremely negative carbon isotope values from the canyon-fill and canyon-lining crusts have a primary marine origin. Previously interpreted deepening upward trends in the canyon fill (used as evidence of a subaerial erosion episode followed by drowning) are suggested to be fining upward trends, caused by the transition from canyon cutting to canyon filling, with the majority of the fill being of deep-water slope origin. The basal conglomeratic canyon-fill sediments represent the last vestiges of the high-energy, deep-water, canyon-erosion environment in which the incisions formed. A deep-water origin for the canyons is consistent with all previous stratigraphic observations of the Wonoka canyons, including the conspicuous lack of regional unconformities in the lower Wonoka Formation, and their emanation from the deep-water facies of the Wonoka Formation. A submarine canyon origin also removes the need for extreme (~ 1 km) relative sea level fluctuation and associated problems (i.e. an enclosed basin with Messinian-style evaporative drawdown or thermal uplift above a migrating mantle plume) required by the subaerial valley hypotheses. 相似文献
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May-Linn Paulsen Andreas J. Andersson Lihini Aluwihare Tyler Cyronak Sydney D’Angelo Charlie Davidson Hany Elwany Sarah N. Giddings Heather N. Page Magali Porrachia Stephen Schroeter 《Estuaries and Coasts》2018,41(4):1050-1068
Estuaries are important subcomponents of the coastal ocean, but knowledge about the temporal and spatial variability of their carbonate chemistry, as well as their contribution to coastal and global carbon fluxes, are limited. In the present study, we measured the temporal and spatial variability of biogeochemical parameters in a saltmarsh estuary in Southern California, the San Dieguito Lagoon (SDL). We also estimated the flux of dissolved inorganic carbon (DIC) and total organic carbon (TOC) to the adjacent coastal ocean over diel and seasonal timescales. The combined net flux of DIC and TOC (FDIC?+?TOC) to the ocean during outgoing tides ranged from ??1.8±0.5?×?103 to 9.5±0.7?×?103?mol C h?1 during baseline conditions. Based on these fluxes, a rough estimate of the net annual export of DIC and TOC totaled 10±4?×?106?mol C year?1. Following a major rain event (36 mm rain in 3 days), FDIC?+?TOC increased and reached values as high as 29.0 ±?0.7?×?103?mol C h?1. Assuming a hypothetical scenario of three similar storm events in a year, our annual net flux estimate more than doubled to 25 ±?4?×?106?mol C year?1. These findings highlight the importance of assessing coastal carbon fluxes on different timescales and incorporating event scale variations in these assessments. Furthermore, for most of the observations elevated levels of total alkalinity (TA) and pH were observed at the estuary mouth relative to the coastal ocean. This suggests that SDL partly buffers against acidification of adjacent coastal surface waters, although the spatial extent of this buffering is likely small. 相似文献
8.
Sarah N. Giddings Derek A. Fong Stephen G. Monismith C. Chris Chickadel Kathleen A. Edwards William J. Plant Bing Wang Oliver B. Fringer Alexander R. Horner-Devine Andrew T. Jessup 《Estuaries and Coasts》2012,35(2):665-681
Estuarine fronts are well known to influence transport of waterborne constituents such as phytoplankton and sediment, yet
due to their ephemeral nature, capturing the physical driving mechanisms and their influence on stratification and mixing
is difficult. We investigate a repetitive estuarine frontal feature in the Snohomish River Estuary that results from complex
bathymetric shoal/channel interactions. In particular, we highlight a trapping mechanism by which mid-density water trapped
over intertidal mudflats converges with dense water in the main channel forming a sharp front. The frontal density interface
is maintained via convergent transverse circulation driven by the competition of lateral baroclinic and centrifugal forcing.
The frontal presence and propagation give rise to spatial and temporal variations in stratification and vertical mixing. Importantly,
this front leads to enhanced stratification and suppressed vertical mixing at the end of the large flood tide, in contrast
to what is found in many estuarine systems. The observed mechanism fits within the broader context of frontogenesis mechanisms
in which varying bathymetry drives lateral convergence and baroclinic forcing. We expect similar trapping-generated fronts
may occur in a wide variety of estuaries with shoal/channel morphology and/or braided channels and will similarly influence
stratification, mixing, and transport. 相似文献
9.
Cloelle G. S. Giddings Fang Liu James M. Gossett 《Ground Water Monitoring & Remediation》2010,30(2):106-113
Chlorinated ethenes such as tetrachloroethene and trichloroethene have been widely used as dry-cleaning and degreasing solvents. Under anaerobic conditions, microorganisms reduce these parent compounds to less-chlorinated daughter products such as cis-1,2-dichloroethene (cDCE), and often further to ethene. This process can be stalled at cDCE, due to insufficient supply of reductants and/or inadequate microbial-community composition. Recently, a novel bacterium, Polaromonas sp. JS666, was isolated that is able to aerobically oxidize cDCE as sole carbon and energy source. As such, it is a promising candidate for use as a subsurface, bioaugmentation agent at sites where anaerobic bioremediation is inappropriate or has stalled and cDCE has migrated to, and accumulated within, aerobic zones, or where it is practical to impose aerobic conditions. Subsurface sediments or groundwater from six such cDCE-contaminated sites were used to construct microcosms. In every sediment or groundwater inoculated with JS666, the organism was able to degrade cDCE, provided that the pH remained circum-neutral. Even when JS666 was challenged with an alternate carbon source, or in the presence of competitive/predatory microorganisms, there was a measure of success. Collectively, these microcosm studies suggest that JS666 is a viable candidate for the bioaugmentation of aerobic, cDCE-contaminated sites. A minimum inoculation level in excess of 105 cells per mL is recommended for field applications. At this level of inoculation, 100 L of inoculum culture grown to an OD600 of 1.0 should be able to treat a 10-m × 30-m × 80-m (24,000-m3) plot. 相似文献
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