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Journal articles on the topic 'Salt pans (Geology) Australia'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Perold, S. M. "Studies in the Sphaerocarpales (Hepaticae) from southern Africa. 1. The genus Monocarpus and its only member, M. sphaerocarpus." Bothalia 29, no. 2 (October 1, 1999): 225–30. http://dx.doi.org/10.4102/abc.v29i2.592.

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A taxonomic account of the genus Monocarpus and its only species, M. sphaerocarpus, is presented. The species was initially discovered on salt pans in Western Australia, and only later, in southern Africa. It is extremely rare and the structure of the minute thalli is difficult to determine, also to describe and to illustrate. As far as could be determined, no SEM micrographs o f the thalli and spores have been published before, nor has the capsule wall been illustrated.

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2

Lou, Pengcheng, Zhongying Miao, Mianping Zheng, Xuefei Zhang, Zhuang Ruan, and Qihui Xu. "Paleogeographic Characteristics of the Mengyejing Formation in the Simao Basin during Its Depositional Period and Its Indication of Potash Mineralization: A Case Study of MZK-3 Well." Minerals 11, no. 4 (March 24, 2021): 338. http://dx.doi.org/10.3390/min11040338.

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In China, pre-Quaternary solid potash deposit has only been discovered in the Simao Basin, and the Lower Cretaceous Mengyejing (MYJ) Formation (Fm.) is the productive layer of potash deposit. In this study, we investigated the clay conglomerates which are distributed in upper and lower members of the potash-bearing salt rock layer. We analyzed the relative contents of major elements (Al2O3, Fe2O3T, MgO, CaO, Na2O, K2O) and trace elements (B, Ba, Co, Cr, Cu, Ga, Mn, Ni, Rb, Sr, V, Zn, Zr) in the samples. The results show that MgO and CaO in the major elements are rich relative to Post Archean A

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3

Hearon, Thomas E., Mark G. Rowan, Timothy F. Lawton, Patrick T. Hannah, and Katherine A. Giles. "Geology and tectonics of Neoproterozoic salt diapirs and salt sheets in the eastern Willouran Ranges, South Australia." Basin Research 27, no. 2 (May 20, 2014): 183–207. http://dx.doi.org/10.1111/bre.12067.

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4

Bechor, B., D. Sivan, S. Miko, O. Hasan, M. Grisonic, I. Radić Rossi, B. Lorentzen, et al. "Salt pans as a new archaeological sea-level proxy: A test case from Dalmatia, Croatia." Quaternary Science Reviews 250 (December 2020): 106680. http://dx.doi.org/10.1016/j.quascirev.2020.106680.

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5

Pierre, Catherine. "Isotopic evidence for the dynamic redox cycle of dissolved sulphur compounds between free and interstitial solutions in marine salt pans." Chemical Geology 53, no. 3-4 (December 1985): 191–96. http://dx.doi.org/10.1016/0009-2541(85)90068-3.

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6

Gannaway Dalton, C. Evelyn, Katherine A. Giles, Mark G. Rowan, Richard P. Langford, Thomas E. Hearon, and J. Carl Fiduk. "Sedimentologic, stratigraphic, and structural evolution of minibasins and a megaflap formed during passive salt diapirism: The Neoproterozoic Witchelina diapir, Willouran Ranges, South Australia." Journal of Sedimentary Research 90, no. 2 (February 20, 2020): 165–99. http://dx.doi.org/10.2110/jsr.2020.9.

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ABSTRACT This study documents the growth of a megaflap along the flank of a passive salt diapir as a result of the long-lived interaction between sedimentation and halokinetic deformation. Megaflaps are nearly vertical to overturned, deep minibasin stratal panels that extend multiple kilometers up steep flanks of salt diapirs or equivalent welds. Recent interest has been sparked by well penetrations of unidentified megaflaps that typically result in economic failure, but their formation is also fundamental to understanding the early history of salt basins. This study represents one of the firs

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7

Street, Gregory J., Gabriella Pracilio, and Ann-Marie Anderson-Mayes. "Interpretation of Geophysical Data for Salt Hazard Identification and Catchment Management in Southwest Western Australia." Exploration Geophysics 33, no. 2 (June 2002): 65–72. http://dx.doi.org/10.1071/eg02065.

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8

Vidal‐Royo, Oskar, Mark G. Rowan, Oriol Ferrer, Mark P. Fischer, J. Carl Fiduk, David P. Canova, Thomas E. Hearon, and Katherine A. Giles. "The transition from salt diapir to weld and thrust: Examples from the Northern Flinders Ranges in South Australia." Basin Research 33, no. 5 (June 23, 2021): 2675–705. http://dx.doi.org/10.1111/bre.12579.

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9

Miller, R. McG, C. Krapf, T. Hoey, J. Fitchett, A.-K. Nguno, R. Muyambas, A. Ndeutepo, A. Medialdea, A. Whitehead, and I. Stengel. "A sedimentological record of fluvial-aeolian interactions and climate variability in the hyperarid northern Namib Desert, Namibia." South African Journal of Geology 124, no. 3 (September 1, 2021): 575–610. http://dx.doi.org/10.25131/sajg.124.0008.

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Abstract The aeolian regime of the 100 km wide, hyperarid Namib Desert has been sporadically punctuated by the deposition of fluvial sediments generated during periods of higher humidity either further inland or well within the desert from Late Oligocene to Late Holocene. Four new Late Cenozoic formations are described from the northern Skeleton Coast and compared with formations further south: the Klein Nadas, Nadas (gravels, sands), Vulture’s Nest (silts) and Uniab Boulder Formations. The Klein Nadas Formation is a trimodal mass-flow fan consisting of thousands of huge, remobilised, end-Carb

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10

Salama, R. B. "Geomorphology, geology and palaeohydrology of the broad alluvial valleys of the Salt River System, Western Australia." Australian Journal of Earth Sciences 44, no. 6 (December 1997): 751–65. http://dx.doi.org/10.1080/08120099708728352.

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11

Counts, John W., and Kathryn J. Amos. "Sedimentology, depositional environments and significance of an Ediacaran salt-withdrawal minibasin, Billy Springs Formation, Flinders Ranges, South Australia." Sedimentology 63, no. 5 (April 1, 2016): 1084–123. http://dx.doi.org/10.1111/sed.12250.

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12

Bierwirth, P. N., and R. S. Brodie. "Gamma-ray remote sensing of aeolian salt sources in the Murray–Darling Basin, Australia." Remote Sensing of Environment 112, no. 2 (February 2008): 550–59. http://dx.doi.org/10.1016/j.rse.2007.05.012.

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13

CATHRO, DONNA L., JOHN K. WARREN, and GEORGE E. WILLIAMS. "Halite saltern in the Canning Basin, Western Australia: a sedimentological analysis of drill core from the Ordovician-Silurian Mallowa Salt." Sedimentology 39, no. 6 (December 1992): 983–1002. http://dx.doi.org/10.1111/j.1365-3091.1992.tb01992.x.

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14

Backé, Guillaume, Graham Baines, David Giles, Wolfgang Preiss, and Andrew Alesci. "Basin geometry and salt diapirs in the Flinders Ranges, South Australia: Insights gained from geologically-constrained modelling of potential field data." Marine and Petroleum Geology 27, no. 3 (March 2010): 650–65. http://dx.doi.org/10.1016/j.marpetgeo.2009.09.001.

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15

Rowan, Mark G., and Bruno C. Vendeville. "Foldbelts with early salt withdrawal and diapirism: Physical model and examples from the northern Gulf of Mexico and the Flinders Ranges, Australia." Marine and Petroleum Geology 23, no. 9-10 (December 2006): 871–91. http://dx.doi.org/10.1016/j.marpetgeo.2006.08.003.

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16

KOVALEVYCH, V., T. MARSHALL, T. PERYT, O. PETRYCHENKO, and S. ZHUKOVA. "Chemical composition of seawater in Neoproterozoic: Results of fluid inclusion study of halite from Salt Range (Pakistan) and Amadeus Basin (Australia)." Precambrian Research 144, no. 1-2 (January 20, 2006): 39–51. http://dx.doi.org/10.1016/j.precamres.2005.10.004.

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17

Munday, T. J., A. J. Hill, T. Wilson, B. Hopkins, A. L. Telfer, G. J. White, and A. Green. "Combining geology and geophysics to develop a hydrogeologic framework for salt interception in the Loxton Sands aquifer, central Murray Basin, Australia." Australasian Journal of Water Resources 9, no. 2 (January 2005): 163–68. http://dx.doi.org/10.1080/13241583.2005.11465274.

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18

Fraser, Melissa B., G. Jock Churchman, David J. Chittleborough, and Pichu Rengasamy. "Effect of plant growth on the occurrence and stability of palygorskite, sepiolite and saponite in salt-affected soils on limestone in South Australia." Applied Clay Science 124-125 (May 2016): 183–96. http://dx.doi.org/10.1016/j.clay.2016.02.012.

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19

Townson, W. G. "THE SUBSURFACE GEOLOGY OF THE WESTERN OFFICER BASIN — RESULTS OF SHELL'S 1980-1984 PETROLEUM EXPLORATION CAMPAIGN." APPEA Journal 25, no. 1 (1985): 34. http://dx.doi.org/10.1071/aj84003.

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The Officer Basin described in this paper includes four Proterozoic to Lower Palaeozoic sub-basins (Gibson, Yowalga, Lennis, Waigen) which extend in a northwest to southeast belt across 200 000 sq. km of central Western Australia. These sub-basins are bounded by Archaean to Proterozoic basement blocks and are almost entirely concealed by a veneer of Permian and Cretaceous sediments. Depth to magnetic basement locally exceeds eight kilometres.Until recently, information on the sub-surface geology was limited to shallow levels, based on the results of a petroleum exploration campaign in the 1960

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20

Clarke, C. J., R. J. George, R. W. Bell, and R. J. Hobbs. "Major faults and the development of dryland salinity in the western wheatbelt of Western Australia." Hydrology and Earth System Sciences 2, no. 1 (March 31, 1998): 77–91. http://dx.doi.org/10.5194/hess-2-77-1998.

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Abstract. Dryland salinity poses a major threat to agricultural production in the wheatbelt of Western Australia and much time and effort is expended on understanding the mechanisms which cause it and on developing techniques to halt or reverse its development. Whilst the location of much dryland salinity can be explained by its topographic position, a significant proportion of it cannot. This study investigated the hypothesis that major faults in the Yilgarn Craton represented in aeromagnetic data by intense curvilinear lows explained the location of areas of dryland salinity not explained by

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21

Carpenter, Kenneth, and Eugene Lindsey. "Redefining the Upper Jurassic Morrison Formation in Garden Park National Natural Landmark and vicinity, eastern Colorado: Geology of the Intermountain West." Geology of the Intermountain West 6 (January 31, 2019): 1–30. http://dx.doi.org/10.31711/giw.v6.pp1-30.

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The Garden Park National Natural Landmark (GPNNL) is north of Cañon City, Colorado, and encompasses all of the major historical dinosaur quarries of the Upper Jurassic Morrison Formation in this area. The formation there can be divided into the lower redefined Ralston Creek Member and an upper unnamed member. The Morrison Formation is bracketed below by the J-5 unconformity and above by the K-1 unconformity. The Ralston Creek Member is composed of up to 55 m of arkosic conglomerate, sandstone, siltstone, and gypsum conformably underlying the unnamed member. Fossil fishes previously used to inf

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22

Carpenter, Kenneth, and Eugene Lindsey. "Redefining the Upper Jurassic Morrison Formation in Garden Park National Natural Landmark and vicinity, eastern Colorado: Geology of the Intermountain West." Geology of the Intermountain West 6 (January 25, 2019): 1–30. http://dx.doi.org/10.31711/giw.v6i0.33.

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The Garden Park National Natural Landmark (GPNNL) is north of Cañon City, Colorado, and encompasses all of the major historical dinosaur quarries of the Upper Jurassic Morrison Formation in this area. The formation there can be divided into the lower redefined Ralston Creek Member and an upper unnamed member. The Morrison Formation is bracketed below by the J-5 unconformity and above by the K-1 unconformity. The Ralston Creek Member is composed of up to 55 m of arkosic conglomerate, sandstone, siltstone, and gypsum conformably underlying the unnamed member. Fossil fishes previously used to inf

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23

Hens, Luc, Nguyen An Thinh, Tran Hong Hanh, Ngo Sy Cuong, Tran Dinh Lan, Nguyen Van Thanh, and Dang Thanh Le. "Sea-level rise and resilience in Vietnam and the Asia-Pacific: A synthesis." VIETNAM JOURNAL OF EARTH SCIENCES 40, no. 2 (January 19, 2018): 127–53. http://dx.doi.org/10.15625/0866-7187/40/2/11107.

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Climate change induced sea-level rise (SLR) is on its increase globally. Regionally the lowlands of China, Vietnam, Bangladesh, and islands of the Malaysian, Indonesian and Philippine archipelagos are among the world’s most threatened regions. Sea-level rise has major impacts on the ecosystems and society. It threatens coastal populations, economic activities, and fragile ecosystems as mangroves, coastal salt-marches and wetlands. This paper provides a summary of the current state of knowledge of sea level-rise and its effects on both human and natural ecosystems. The focus is on coastal urban

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24

Souza, Ian Cerdeira de Oliveira, Guilherme Augusto Mendonça Maia, Narelle Maia de Almeida, João Capistrano Abreu Neto, and George Satander Sá Freire. "Sedimentary Dynamic and Composition of a Tidal Channel in a Tropical Hot Semi-Arid Environment, NE Brazil." Anuário do Instituto de Geociências - UFRJ 43, no. 4 (December 18, 2020). http://dx.doi.org/10.11137/2020_4_144_155.

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Tidal channels comprise a peculiar and dynamic environment. This paper aims to recognize the sedimentary distribution and composition of a tidal channel located in a semi-arid climate area in order to understand the sedimentary dynamics of the region. This region has economic and environmental importance considering that several activities are developed in the area such as; salt industry and aquaculture with shrimp farming. The results and discussion presented here on the Barra Grande Port tidal channel are based on 43 superficial samples distributed in the area, in which we analyzed the grain

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25

LEMAR, ROBERT, and JOHN WARREN,* Na. "The Influence of Salt Structure Movement on Potential Reservoir Occurrence in the Bonaparte Basin, Northwest Shelf, Australia." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8fc46-1712-11d7-8645000102c1865d.

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26

Pirajno, Franco. "Mineral systems and their putative link with mantle plumes." Geological Society, London, Special Publications, May 5, 2021, SP518–2020–276. http://dx.doi.org/10.1144/sp518-2020-276.

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AbstractIn this contribution, I discuss the putative link of mantle plumes with selected categories of mineral systems. Continental rifting and break-ups can be induced by the upwelling of mantle plumes, also resulting in the generation of a wide range of mineral deposits. These include magma-associated ores, anorogenic igneous events responsible for iron oxide–copper–gold (IOCG) deposits, carbonatites and hydrothermal-induced mineralization, as well as hydrocarbons, salt domes, petroleum and gas, and several mineral systems in continental passive margins. Amongst the magma-associated mineral

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