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1

Santos, Luís Filipe Fernandes dos. "Calcretos no Alentejo - Contributo para a sua caracterização geotécnica." Master's thesis, Faculdade de Ciências e Tecnologia, 2013. http://hdl.handle.net/10362/11882.

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Dissertação para obtenção do Grau de Mestre em Engenharia Geológica<br>Os calcretos são depósitos importantes normalmente associados a climas semi-áridos, resultando, em regra, de carbonatação superficial devido ao contacto com água carbonatada estagnada e sua infiltração nas superfícies de fraqueza das rochas encaixantes. Existem, no entanto, exemplos de carbonatação associada a águas subterrâneas, onde a circulação interna de fluxos de água, eventualmente até associados a actividade hidrotermal tardia relacionada com a instalação de maciços ígneos, que conjugada com condições climáticas p
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2

Brasier, Alexander Thomas. "Palaeoenvironmental reconstructions from Quaternary tufas and calcretes, central Greece." Thesis, University of East Anglia, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.437889.

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3

Krug, Mark Alan. "Geochemical exploration in calcrete terrains." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1006891.

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This work takes a look at some of the literature on calcretes and especially the problem of geochemical exploration in calcrete terrains. The conclusion that will be reached is that exploration in calcrete terrains is not futile and that provided the explorationist is aware of the types of calcrete and their genetic implications calcrete can be used as a sampling medium and anomalies can be detected through calcrete (p.1.)<br>KMBT_363<br>Adobe Acrobat 9.54 Paper Capture Plug-in
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Cunha, Paola Viana de Castro. "Gênese de Calcretes da formação Guabirotuba, Bacia de Curitiba, Paraná." reponame:Repositório Institucional da UFPR, 2012. http://hdl.handle.net/1884/26941.

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Resumo: A Bacia de Curitiba (Mioceno-Pleistoceno) tem área atual aproximada de 3000 km². Coincide parcialmente com a região metropolitana da cidade homônima, situada no Sul do país. A bacia constitui depressão alongada de direção ENE, pertencente ao Sistema de Riftes Cenozóicos do Sul e Sudeste do Brasil. A Formação Guabirotuba, principal unidade sedimentar da bacia, é constituída por areias arcosianas localmente conglomeráticas e lamas, acumuladas sobre embasamento de rochas metamórficas e ígneas pré-cambrianas. Corresponde a depósitos de leques aluviais coalescentes e rios entrelaçados. Em a
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Santos, Ana Luísa Sebastião Rodrigues dos. "Geoquímica, mineralogia e luminescência de um mundo pré-histórico em negativo: do neolítico à idade do bronze região do Alentejo." Doctoral thesis, Universidade de Aveiro, 2015. http://hdl.handle.net/10773/14828.

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Doutoramento em Geociências<br>Os trabalhos de investigação arqueológica realizados nos últimos anos no Sul de Portugal têm revelado a existência de estruturas arqueológicas negativas com arquiteturas e funcionalidades inéditas, que levantaram questões quanto à sua dinâmica de preenchimento e cronologia. Estas estruturas (fossos, fossas e hipogeus) estão associadas a sociedades Pré-Históricas, do Neolítico à Idade do Bronze, e foram escavadas em formações carbonatadas e materiais de alteração de granitos, e de dioritos e gabros associados. Neste trabalho estudaram-se diferentes fracções granu
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6

Pfeiffer, Jakob Marco. "Evolución y Génesis de Calcretas Pedogénicas en la Paleobahía de Tongoy." Tesis, Universidad de Chile, 2011. http://www.repositorio.uchile.cl/handle/2250/102582.

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7

Phillips, Graham Mark. "Fracture cements and cementation processes in the Devonian-Carboniferous Clair group and underlying Lewisian basement, West of Shetland." Thesis, University of Aberdeen, 1995. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU078080.

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Clair Groups and underlying basement contain cataclastic faults, cement-sealed faults/veins and open fractures. The dominant fracture cements are calcite and pyrite, although fluorite (with sulphides and native silver) occurs in minor amounts in some Clair Group fractures, marcasite is often associated with Clair Group fracture-hosted pyrite, and some basement fractures contain epidote/chlorite and quartz/feldspar/hematite. Calcite cements in many Clair Group fractures may have crystallised from porewaters whose calcium and bicarbonate were mostly remobilised from Clair Group calcretes. Many o
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8

Oliveira, Emiliano Castro de. "Tufas calcárias da Serra da Bodoquena, MS." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-05062009-112215/.

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Aflorando abundantemente nas drenagens da Serra da Bodoquena, região sudoeste do Estado de Mato Grosso do Sul, os depósitos de tufas calcárias, descritos como a porção superior da Formação Xaraiés, representam o mais notável depósito do tipo no Brasil, devido à variedade de formas. Sendo a maior atração do pólo eco-turístico de Bonito, MS, as tufas calcárias apresentam-se sob formas de barragens, cachoeiras e depósitos de micritos inconsolidados, que por sua vez geram as piscinas naturais e quedas dágua tão procuradas pelos turistas. Mesmo com tamanha importância, tal rocha não havia recebido
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9

Quast, Andres. "Calcretes aus jungpaläozoischen Bodenbildungen ein möglicher Proxy für die CO2-Konzentration der Paläoatmosphäre /." [S.l.] : [s.n.], 2003. http://webdoc.sub.gwdg.de/diss/2003/quast/quast.pdf.

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10

Oliveira, Emiliano Castro de. "Rochas carbonáticas continentais (Quaternário) do Pantanal Matogrossense e adjacências." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-14112013-111133/.

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Os carbonatos continentais vêm sendo bastante estudados nos últimos anos, devido ao seu potencial como arquivo paleoclimáticoe, mais recentemente, como rocha reservatório de hidrocarbonetos. Carbonatos continentais quaternários são registrados na serra da Bodoquena e no platô Corumbá/Ladário, adjacências da Bacia do Pantanal, no Estado de Mato Grosso do Sul,bem como na serra das Araras, Mato Grosso. O estudo desses depósitos é deinteresse científico, uma vez que eles podem contribuir como análogos para ocorrências de carbonatos continentais mais antigos, bem como servir como objeto de a
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Candy, Ian. "Quaternary climate change and landform development in southeast Spain : U-series dating of calcretes." Thesis, University of Reading, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.414519.

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12

Grevenitz, Paul. "The character and genesis of pedogenic calcrete in southern Australia." Access electronically, 2006. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20061206.141643/index.html.

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13

Saccò, Mattia. "Functional ecology of calcrete aquifers in arid zone Western Australia." Thesis, Curtin University, 2020. http://hdl.handle.net/20.500.11937/80356.

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This study investigates the ecology of an arid zone calcrete through an interdisciplinary design composed of multivariate analyses, hydrology, isotopic ecology and genetics. Our results indicate that the biotic community (microbes and stygofauna) is closely linked to the hydrodynamic conditions influenced by different rainfall regimes. The inflow of rainfall triggered shifts towards more deterministic dynamics, revealing a complex web of interactions. This investigation provides crucial untangling of the ecological dynamics regulating biotic communities in groundwaters.
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Borges, S?rgio Vieira Freire. "Calcretes pedog?nicos ao longo de sistemas de fraturas e acamamentos em carbonatos neoproteroz?icos da Bacia de Irec?, Estado da Bahia." PROGRAMA DE P?S-GRADUA??O EM CI?NCIA E ENGENHARIA DE PETR?LEO, 2016. https://repositorio.ufrn.br/jspui/handle/123456789/21957.

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Maoski, Eloir. "Gênese dos calcretes da Formação Marília no Centro-Oeste Paulista e Triângulo Mineiro, Bacia Bauru (Ks)." reponame:Repositório Institucional da UFPR, 2012. http://hdl.handle.net/1884/27326.

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Resumo: A Bacia Bauru desenvolveu-se na Plataforma Sulamericana após a ruptura do Gondwana no Cretáceo Superior. Foi preenchida por sequência siliciclástica predominante arenosa na forma de leques aluviais de borda, sistemas de rios entrelaçados, extensos lençóis de areia eólicos e deserto interior. Hoje, tal sequência suprabasáltica tem cerca de 480m de espessura e seu relevo está em estágio de dissecação. A Formação Marília do Grupo Bauru tem a mais expressiva ocorrência de calcrete dentre as unidades litoestratigráficas da bacia, além de registros de paleossolos e ocorrências fossilíferas d
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Shaw, Alexander Iain. "The characterisation of calcrete based on its environmental settings within selected regions of the Kalahari, Southern Africa." Thesis, University of Oxford, 2009. http://ora.ox.ac.uk/objects/uuid:3474d9e4-fa10-4bd4-af7e-dcbe9ebad640.

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Chemical sediments in a variety of geomorphic environments (pedogenic, fluvial, palustrine, lacustrine and pan) were investigated from seven regions (SW Kalahari, Kgalagadi, Kalkweissrand, Etosha, Linyanti, Okavango and Ngami) in the Kalahari of southern Africa. These primary and multi-phase sediments were characterised by a range of pure and intergrade silcrete, calcrete and dolocrete fabrics which contained an array of structures indicative of the crystalline and biogenic processes responsible for their precipitation, epigenesis and paragenesis. Petrography, mineralogy and isotope geochemist
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Phillips, Sally Elizabeth. "The interaction of geological, geomorphic and pedogenic processes in the genesis of calcrete." Title page, table of contents and abstract only, 1988. http://hdl.handle.net/2440/19052.

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18

Akinyemi, Segun Ajayi. "Optimisation of selective extraction techniques as a tool for geochemical mapping in the Southern Africa region." Thesis, University of the Western Cape, 2008. http://etd.uwc.ac.za/index.php?module=etd&action=viewtitle&id=gen8Srv25Nme4_3444_1260521237.

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<p>The complex nature and composition of regolith cover in Southern Africa is a major challenge to geochemical mapping for concealed mineralization. Some of the setbacks to successful geochemical exploration may be ascribed to the use of various partial extraction techniques,without a profound understanding of the regolith components and their composition. This investigation therefore focuses on the use of hydroxylamine partial extraction geochemistry for geochemical mapping in regolith over two contrasting environments viz<br>aeolian sand-calcrete regolith over Au mineralization at Amalia Blu
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Verrecchia, Eric. "Le role de la sedimentation, de l'activite biologique et de la diagenese dans l'edification des nari-calcretes de nazareth (galilee, israel)." Paris 6, 1992. http://www.theses.fr/1992PA066627.

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L'etude sedimentologique, geochimique, petrophysique et petrographique d'un encroutement carbonate de galilee a montre qu'il etait constitue, de bas en haut, d'un facies d'alteration du substrat crayeux sur lequel il repose, d'un depot colluvial de versant, de la racine d'un paleosol et d'une croute zonaire qui scelle le profil. La complexite des microfacies et des ciments revele une evolution polyphasee ou phenomenes diagenetiques precoces (dessiccation, cimentation) et tardifs (induration) interferent. La croute zonaire est un horizon biologique d'origine cyanophytique, se formant au contact
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20

Roulin, François. "L'Eocène continental du synclinal d'Apt (Vaucluse, sud-est de la France) : enchaînements silcrete-calcrete et argilogenèse." Lyon 1, 1985. https://tel.archives-ouvertes.fr/tel-00795051.

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Dans le bassin d' Apt, la série détritique continentale paléocène-éocène est représentée par des sables colorés azoïques, "pro parte" conglomératiques : à la base, l'ensemble inférieur d'âge paléocène à éocène inférieur, vers le haut, l'ensemble supérieur d'âge éocène s. L. Les ensembles inférieur et supérieur montrent une évolution verticale nette des populations argileuses. A cette argilogenèse se superposent deux phases d'altération de surface, la première phase est silicifiante, la deuxième phase est calcitisante. L'alternance de ces transformations avec des phases de dépôts détritiques en
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Lintern, Melvyn John. "The role of biological and non-biological factors in the formation of gold anomalies in calcrete." Thesis, Curtin University, 2011. http://hdl.handle.net/20.500.11937/2174.

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Calcrete has been shown to contain significant Au, derived from nearby mineralisation, and this has led to its current use as an exploration sampling medium. Calcretes are secondary carbonates, principally consisting of calcite and dolomite that may precipitate in regolith in a semi-arid climate. They overprint existing regolith material and commonly contain this material (e.g. soil, colluvium, laterite, saprolite and rock) on, and within, which they form. Vadose (pedogenic) and phreatic (formed by groundwater) are the two principal types of calcrete. Pedogenic calcretes are those that form in
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Roulin, François. "L'Eocène continental du synclinal d' Apt (Vaucluse, Sud-ouest de la France): enchaînements silcrete-calcrete et argilogenèse." Phd thesis, Université Claude Bernard - Lyon I, 1985. http://tel.archives-ouvertes.fr/tel-00795051.

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Dans le bassin d' Apt, la série détritique continentale paléocène-éocène est représentée par des sables colorés azoïques, "pro parte" conglomératiques : à la base, l'ensemble inférieur d'âge paléocène à éocène inférieur, vers le haut, l'ensemble supérieur d'âge éocène s.l. Les ensembles inférieur et supérieur montrent une évolution verticale nette des populations argileuses. A cette argilogenèse se superposent deux phases d'altération de surface, la première phase est silicifiante, la deuxième phase est calcitisante. L'alternance de ces transformations avec des phases de dépôts détritiques en
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23

Silva, Suely Andrade da. "Accelerated change of limestone beige Bahia: a your loss prediction test intensity bright in fachadas under conditions tropical metropolitan in coastal edges." Universidade Federal do CearÃ, 2015. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=14988.

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CoordenaÃÃo de AperfeÃoamento de Pessoal de NÃvel Superior<br>The mineralogical composition of the Beige Bahia (BB) limestone was characterized by petrographic analysis, XRD, total-rock (TR) chemical analysis, and SEM on figurative elements of lytic texture. The results demonstrated that this type of calcrete is dolomitic (dolomite > 10% in TR), reaching over 50% in its lumpy features. The matrix is primarily calcite, whereas quartz (< 5% TR) and palygorskite are the most common accessory minerals. The changing mechanisms of the BB, as a building covering, were investigated from the loss of br
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Kucukuysal, Ceren. "Paleoclimatological Approach To Plio-quaternary Paleosol-calcrete Sequences In Bala And Golbasi (ankara) By Using Mineralogical And Geochemical Proxies." Phd thesis, METU, 2011. http://etd.lib.metu.edu.tr/upload/12613876/index.pdf.

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The major goal of this study is to define the paleoclimatic conditions in Ankara region during Plio-Pleistocene period by evaluating the mineralogical and geochemical proxies carried from the paleosols and their calcretes. The field observations, mineralogical, micromorphological, geochemical and stable isotope investigations were all conducted to achieve a paleoclimatic approach. As pedogenic minerals in calcretes, presence of dolomite with palygorskite in the Karahamzali section and calcite with palygorskite in the Bala section together with high salinity and calcification values reveal the
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Medley, Erica. "Ancient Cataclysmic Floods in the Pacific Northwest: Ancestors to the Missoula Floods." PDXScholar, 2012. https://pdxscholar.library.pdx.edu/open_access_etds/581.

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Ancient Cataclysmic Floods were the Ice Age Floods that left erosional and depositional features and preceded the Missoula Floods (15-18,000 ka) in the Pacific Northwest of the United States (Allen et al., 2009). All previously studied ancient sites were visited (14) and new sites (11) were found; four Missoula Flood quarries were also visited; a total of 29 sites were studied in this thesis. The use of calcrete paleosols to provide relative age dates for flood deposits was analyzed in this thesis. Missoula Flood gravel pits were sampled in order to examine the degree of calcrete development i
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MACEDO, Andréia Oliveira. "Estudo geoarquiológico dos níveis arenoso e de cascalheira cimentada por concreção carbonática do Sítio Lagoa Uri de Cima, Salgueiro-PE." Universidade Federal de Pernambuco, 2016. https://repositorio.ufpe.br/handle/123456789/17988.

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Baufeldt, Sven. "A reconciliation study of different resource estimation methods and drill hole spacing as applied to the Langer Heinrich calcrete-hosted uranium deposit, Namibia." Thesis, Rhodes University, 2018. http://hdl.handle.net/10962/62527.

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The Langer Heinrich calcrete hosted uranium deposit is situated approximately 90 km to east of the coastal town of Swakopmund in Namibia. It is run by an Australian owned company, Paladin Energy Limited, along with China National Nuclear Corporation (CNNC) who maintain 25% of the shares. Production commenced in 2007 and has been ongoing. Carnotite is the primary and only ore mineral, and the nature of mineralisation within the Langer Heinrich palaeo channel dictates westward-directed continuous open pit mining. Smaller-scale 1micro pits target near-surface, high-grade, lenses toward the east.
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Fabris, Adrian. "Modelling the origins of the Regolith and Calcrete anomalies at the KO1 and KO4 prospects in the Kimba Region, with implications for gold mineralisation /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SB/09sbf128.pdf.

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Silva, Suely Andrade da. "Alteração acelerada do calcário bege Bahia: um ensaio de predição de perda de sua intensidade de brilho em fachadas sob condições tropicais metropolitanas, em orlas litorâneas." reponame:Repositório Institucional da UFC, 2015. http://www.repositorio.ufc.br/handle/riufc/20121.

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SILVA, Suely Andrade da. Alteração acelerada do calcário bege Bahia: um ensaio de predição de perda de sua intensidade de brilho em fachadas sob condições tropicais metropolitanas, em orlas litorâneas. 2015. 150 f. Tese (Doutorado em geologia)- Universidade Federal do Ceará, Fortaleza-CE, 2015.<br>Submitted by Elineudson Ribeiro (elineudsonr@gmail.com) on 2016-10-11T18:47:15Z No. of bitstreams: 1 2015_tese_sasilva.pdf: 5201692 bytes, checksum: 1f86f9b8f74228acdda8000b08836ad5 (MD5)<br>Approved for entry into archive by Jairo Viana (jairo@ufc.br) on 2016-10-11T23:38:49Z (GMT) No. of bitstreams:
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Ayers, James D. "Lithologic Evidence of Jurassic/Cretaceous Boundary Within the Nonmarine Cedar Mountain Formation, San Rafael Swell, Utah." Ohio University / OhioLINK, 2004. http://www.ohiolink.edu/etd/view.cgi?ohiou1097256637.

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Solomon, Henok Goitom. "Application of multivariate statistics and Geographic Information Systems (GIS) to map groundwater quality in the Beaufort West area, Western Cape, South Africa." Thesis, UWC, 2013. http://etd.uwc.ac.za/index.php?module=etd&action=viewtitle&id=gen8Srv25Nme4_4718_1395924268.

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<p><font face="TimesNewRomanPSMT"> <p align="left">Groundwater in arid and semi-arid areas like the Karoo region of South Africa is an important source of domestic, agricultural and industrial source of fresh water. As a scarce resource, it requires extensive quality control and protection through innovative methods and efficient strategies. The town of Beaufort West and its vicinity use groundwater as a major source of municipal and private water supply. Forty nine groundwater samples were collected from spatially referenced boreholes located in and around the town of Beaufort West and were a
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Lepetit, Petra [Verfasser]. "Kohlenstoff-Isotopie miozäner Calcretes in Kappadokien (Türkei) / von Petra Lepetit." 2010. http://d-nb.info/1011404869/34.

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Tylkowski, L. N. "Origin and genesis of calcrete in the Murray Basin." Thesis, 2004. http://hdl.handle.net/2440/123592.

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This item is only available electronically.<br>Calcretes and other terrestrial carbonate accumulations have formed throughout the Murray Basin during the Quaternary, particularly in far western regions. Ooids and grain coatings of CaCO3 by infiltrating carbonate saturated solutions indicate calcrete has formed through pedogenic processes. Based on different morphologies and spatial relationships calcretes historically have been identified as either the younger Bakara or older Ripon Calcrete. The congruence of different stratigraphic calcretes, particularly the Bakara and Ripon Calcretes, wa
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Javidkar, Seyedmohammad. "Molecular systematics and biogeographic history of oniscidean isopod troglofauna in groundwater calcretes of Central Western Australia." Thesis, 2014. http://hdl.handle.net/2440/93518.

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Groundwater calcretes of central Western Australia have revealed an extraordinary diversity of short-range endemic invertebrate subterranean fauna. Although considerable attention has been given to the aquatic dwellers of the calcretes (stygofauna), the subterranean terrestrial fauna of the calcretes (troglofauna), particularly the oniscidean isopods, have been poorly studied. This thesis, including four data chapters, presents the results of multiple-gene and morphological analyses to establish a phylogenetic framework for elucidation of species diversity, systematics, and the biogeographic h
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Quast, Andres. "Calcretes aus jungpaläozoischen Bodenbildungen - ein möglicher Proxy für die CO2-Konzentration der Paläoatmosphäre." Doctoral thesis, 2003. http://hdl.handle.net/11858/00-1735-0000-0006-B31B-5.

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Quast, Andres [Verfasser]. "Calcretes aus jungpaläozoischen Bodenbildungen : ein möglicher Proxy für die CO2-Konzentration der Paläoatmosphäre / vorgelegt von Andres Quast." 2003. http://d-nb.info/968506887/34.

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37

Phillips, Sally Elizabeth. "The interaction of geological, geomorphic and pedogenic processes in the genesis of calcrete." Thesis, 1988. http://hdl.handle.net/2440/19052.

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The term'calcrete' encompasses any secondary carbonate accumulation found within the regolith, irrespective of morphology and degree of induration: Calcretes cover geographically extensive areas of southern Australia as calcareous soils, surficial deposits of carbonate-rich sediment, and calcareous palaeosols. Combined field and laboratory studies of calcretes on the eastern margin of the St Vincent Basin were undertaken to ascertain the mechanisms responsible for calcrete genesis. Geological processes were very important in the development of the Pleistocene carbonate mantle which blankets a
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Klingberg, L. L. "Regolith-landforms and regolith geochemistry of the ‘Tomahawk’ Au-in-calcrete anomaly: Tunkillia, Gawler Craton, South Australia." Thesis, 2009. http://hdl.handle.net/2440/129278.

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This item is only available electronically.<br>The ‘Tomahawk’ Au-in-calcrete anomaly is a zone of peak Au-in-calcrete content within the Tunkillia prospect of the central Gawler Craton, South Australia. Exploration drilling of this area has failed to intersect significant underlying mineralisation, making this an important setting to investigate controls on linkages between Au-in-calcrete expression and possible mineralisation sources. This study is the first to consider the multi-element geochemical characteristics of calcretes at ‘Tomahawk’ rather than using the Au-only approach of previou
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39

Wittwer, P. D. "Geology and geochemistry of regolith carbonate accumulations of the southwestern Curnamona Province, SA: Implications for mineral exploration." Thesis, 2004. http://hdl.handle.net/2440/123526.

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This item is only available electronically.<br>Although regolith carbonate accumulations (RCAs) have been extensively used in mineral exploration programs in the regolith-dominated terrains of the Yilgarn and Gawler Cratons, their use has so far been limited within the Curnamona Province, SA. This study shows how the detailed characterisation of RCAs in the southwestern Curnamona Province enhances their use in mineral exploration programs at the regional to prospect scales. A regional RCA distribution map for the study area shows that RCAs are generally widespread, although certain RCA morph
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40

Dart, Robert C. "Gold-in-calcrete: a continental to profile scale study of regolith carbonates and their association with gold mineralisation." Thesis, 2009. http://hdl.handle.net/2440/61507.

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Regolith carbonate, especially when indurated (calcrete), has been widely adopted as a sampling medium by many Australian Au exploration companies. Rapid uptake of the medium in geochemical exploration programs, following its reported success in the South Australia Challenger Au deposit discovery, has resulted in poorly constrained sampling methodology with many inconsistencies. Results have therefore been equivocal. This study of regolith carbonates and their association with Au will improve this situation. Three aspects of regolith carbonate development and association with Au are inve
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41

Wolff, Keryn Dianne. "Regional Carbonate Geochemistry and Biogeochemistry for Cu Exploration on the Yorke Peninsula, South Australia." Thesis, 2018. http://hdl.handle.net/2440/120233.

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This thesis describes the geochemistry from carbonate rocks and biogeochemistry from mallee across the Yorke Peninsula to better characterise and define mineral systems that may occur in IOCG prospective basement rocks masked by various overlying cover sequences. Presented here is geochemical data from three cliff escarpments (vertical geochemical profiles) which preserve cover sequences overlying basement rocks. Ca/Sr ratios were found to be a defining discriminator between marine and pedogenic carbonate rocks within the profiles; pedogenic carbonates have Ca/Sr ratios less than 650 and marin
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42

Johannsmeier, Anne Elisabeth. "Seed bank strategies in a Kalahari ecosystem in relation to grazing and habitats." Diss., 2009. http://hdl.handle.net/2263/28892.

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The seed bank dynamics of five habitats as well as a grazing gradient in the southwestern Kalahari, South Africa were studied. Soil samples were collected in the following habitats: dune crests, dune slopes, dune streets, a calcrete outcrop and a riverbed on the farm Alpha. Soil samples were also collected along a grazing gradient from a watering point. Three methods of soil seed bank analysis were used to analyse the soil samples and to gain insight into soil seed bank response to habitat type and to grazing pressure, over four seasons in the year 2004. Results from the three methods of analy
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43

McEntegart, L. B. "Gold mobility within dune systems on the Barns property, Wudinna, South Australia: a partial extraction approach." Thesis, 2004. http://hdl.handle.net/2440/122414.

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This item is only available electronically.<br>Regolith carbonate is an established sampling medium in Au exploration. It has a demonstrated correlation with Au content in south western Australia and was the prime indicator in the discovery of the Barns Au prospect Eyre Peninsula, South Australia. Whole rock ICP-MS, AAS and XRF analyses on samples from regolith drill cores and a trench cut into an aeolian sand dune on the Barns prospect established a correlation of Au content (≤17 ppb) with Ca, K, Al and Mg. XRD whole rock and mineral-separate analyses identified calcite, smectite and anker
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