Ore and Alteration Types of the Gold and Copper Mineralization in the Lascogon Project, Surigao del Norte, Mindanao Island, Philippines     

Jonelle Nikolai Crisostomo    Jeddalyn Parian    Daizo Ishiyama    Redempta Baluda    Sonia Eguia    Jocelyn Galapon    Gerry Comia    Jessie Segura    Maureen Laroco    Noel Oliveros  Victor B. Maglambayan 《Resource Geology》2007,57(2):241-247

Two ore and three alteration types were identified in the Lascogon Project of Philex Gold Philippines, in Surigao del Norte, Mindanao Island, Philippines. The jasperoid ore is the host to the Carlin‐like gold mineralization in the Lascogon and Danao prospects. The ore occurs in a decalcified and silicified horizon, with minor chlorite and goethite, stibnite, pyrite and quartz crystals ranging from cryptocrystalline to botryoidal. The stringer–stockwork type Cu‐Au mineralization in the Suyoc prospect is hosted in argillized andesitic rocks of the Mabuhay Formation. The primary ore minerals are chalcopyrite with minor amounts of sphalerite. The alteration types identified are propylitic alteration, argillic alteration and silicification. The propylitized basaltic and andesitic flows of the Bacuag Formation bound the jasperoid mineralization in the Lascogon prospect. Stratigraphically, the relationship between propylitized basalts and stringer–stockwork Cu‐Au is not clear but a lateral change can be inferred from jasperoid in the center and stringer–stockwork towards the east.  相似文献   

Accurate time–frequency–wavenumber analysis to study coda waves     

Estelle Schisselé  Jocelyn Guilbert  Stéphane Gaffet  Yves Cansi 《Geophysical Journal International》2004,158(2):577-591

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Sustainability,development and rural aboriginal communities     

Jocelyn Davies  Elspeth Young 《The Australian geographer》1995,26(2):150-155

Aborigines, because of their population numbers and increasing control over land and resources, are crucial to the sustainable development of rural Australia. However, appropriate Aboriginal development requires the replacement of the ‘top‐down’ approaches generally adopted by government agencies by ‘bottom‐up’ approaches reflecting the needs and aspirations of rural Aboriginal people. Past experience demonstrates that Aborigines have faced many frustrations in reconciling these concepts. But some approaches now being adopted in the use and management of Australia's rangelands provide interesting alternatives which may be more generally applicable in enhancing rangeland sustainability. Examples include land‐use practices conducted by Aborigines living in remote homeland centres on their own freehold land, and the diversity of land uses introduced on pastoral stations now under Aboriginal ownership. Broader recognition of the value of these approaches will depend on widespread acknowledgment of the overall worth of Aboriginal land management knowledge in rural restructuring  相似文献   

Bathymetry and Canyons of the western Solomon Sea     

H. L. Davies  J. B. Keene  K. Hashimoto  M. Joshima  J. E. Stuart  D. L. Tiffin 《Geo-Marine Letters》1986,6(4):181-191

The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m.  相似文献   

Laboratory scale study of an industrial phosphate and thermal treatment for polluted dredged sediments   总被引：1，自引：0，他引：1  

Souhila KRIBI  Jocelyn RAMAROSON  Ange NZIHOU  Patrick SHARROCK  Guy DEPELSENAIRE 《国际泥沙研究》2012,27(4):538-546

Dredged sediments are being chemically treated with phosphoric acid on an industrial scale.The effectiveness of the treatment was evaluated by performing the chemical reaction in a tubular reactor, followed by convective drying and maturation of the treated sediment at ambient temperature and finally thermal destruction of the organic matter by calcinations(500℃-900℃).The influence of acid concentration and calcination temperature on the specific surface area of the sediment was investigated. The stabilization of the heavy metals was evaluated by leaching tests and sequential extraction procedures.The phosphoric acid treatment is effective in reducing heavy metal mobility,a prerequisite for recycling the sediments in various construction materials.  相似文献   

The 1995–96 decline of R Coronae Borealis: high-resolution optical spectroscopy     

N. Kameswara Rao  David L. Lambert  Mark T. Adams  David R. Doss  Guillermo Gonzalez  Artie P. Hatzes  C. Renée James  C. M. Johns-Krull  R. Earle Luck  Gajendra Pandey  Klaus Reinsch  Jocelyn Tomkin  Vincent M. Woolf 《Monthly notices of the Royal Astronomical Society》1999,310(3):717-744

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Compositional characteristics and geodynamic significance of late Miocene volcanic rocks associated with the Chah Zard epithermal gold–silver deposit,southwest Yazd,Iran          下载免费PDF全文

Majid Ghaderi  Mohammad Hashem Emami  Sebastien Meffre  Vadim Kamenetsky  Jocelyn McPhie  Khin Zaw  Rasoul Nasiri Bezenjani 《Island Arc》2018,27(1)

Whole‐rock geochemical and Sr–Nd isotopic data are presented for late Miocene volcanic rocks associated with the Chah Zard epithermal Au–Ag deposit in the Urumieh‐Dokhtar Magmatic Arc (UDMA), Iran, to investigate the magma source, petrogenesis and the geodynamic evolution of the study area. The Chah Zard andesitic to rhyolitic volcanic rocks are characterized by significant Large Ion Lithophile Element (LILE) and Light Rare Earth Element (LREE) enrichment coupled with High Field Strength Element (HFSE) depletion. Our geochemical data indicate an adakitic‐like signature for the volcanic rocks (e.g. SiO₂ > 62 wt%, Al₂O₃ > 15 wt%, MgO < 1.5 wt%, Sr/Y > 70, La/Yb > 35, Yb < 1 ppm, and Y < 18 ppm, and no significant Eu anomalies), distinguishing them from the other volcanic rocks of the UDMA. The Chah Zard volcanic rocks have similar Sr and Nd isotopic compositions; the ⁸⁷Sr/⁸⁶Sr(i) ratios range from 0.704 902 to 0.705 093 and the ε_Nd(i) values are from +2.33 to +2.70. However, the rhyolite porphyry represents the final stage of magmatism in the area and has a relatively high ⁸⁷Sr/⁸⁶Sr ratio (0.705 811). Our data suggest that the andesitic magmas are from a heterogeneous source and likely to result from partial melting of a metasomatized mantle wedge associated with a mixture of subducted oceanic crust and sediment. These melts subsequently underwent fractional crystallization along with minor amounts of crustal assimilation. Our study is consistent with the model that the volcanic host rocks to epithermal gold mineralization in the UDMA are genetically related to late Miocene Neo‐Tethyan slab break‐off beneath Central Iran.  相似文献   

Seismic vulnerability assessment of urban environments in moderate-to-low seismic hazard regions using association rule learning and support vector machine methods   总被引：2，自引：2，他引：0  

Ismaël Riedel  Philippe Guéguen  Mauro Dalla Mura  Erwan Pathier  Thomas Leduc  Jocelyn Chanussot 《Natural Hazards》2015,76(2):1111-1141

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Plio‐Pleistocene tectonics and eustasy in the Gippsland Basin,southeast Australia: Evidence from magnetic imagery and marine geological data     

G. R. Holdgate  M. W. Wallace  S. J. Gallagher  A. J. Smith  J. B. Keene  D. Moore 《Australian Journal of Earth Sciences》2013,60(3):403-426

The Pliocene and Pleistocene sediments of the Gippsland shelf are dominated by mixed carbonates and siliciclastics. From a detailed stratigraphic study that combines conventional marine geology techniques with magnetic imagery, the Late Neogene tectonic and eustatic history can be interpreted and correlated to the onshore section. Stratigraphic analyses of eight oil and gasfield foundation bores drilled to 150 m below the seabed revealed three principal facies types: (i) Facies A is fine‐grained limestone and limey marl deeper than 50 m below the seabed, of Late Pliocene age (nannofossil zones CN11–12); (ii) Facies B is a fine‐coarse pebble quartz‐carbonate sand that occurs 10–50 m below the seabed in the inner shelf, grading down into Facies A in wells in the outer shelf, and is of Early‐Middle Pleistocene age (nannofossil subzones CN13a-14b: ca 1.95–0.26 Ma); and (iii) discontinuous horizons of Facies C composed of carbonate‐poor carbonaceous and micaceous fine quartz sand occurring 10–50 m below the seabed. The sparse benthic foraminifers in Facies C are inner shelf or Gippsland (euryhaline) Lakes forms. Holocene sands dominate the upper 1.5–2.5 m of the Gippsland shelf and disconformably overlie cemented limestones with aragonite dissolution, indicating previous exposure to meteoric water. Nannofossil dating of the limestones indicates ages within subzone CN14b (dated between ca 0.26 and 0.47 Ma). Airborne magnetic imaging across the Gippsland shelf and onshore provides details of buried magnetic palaeoriver channels and barrier systems. The river systems trend south‐southeast from the Snowy, Tambo, Mitchell, Avon, Macalister and Latrobe Rivers across the shelf. Sparker seismic surveys show the magnetic palaeochannels as seismic ‘smudges’ 20–40 m below the seabed. They appear to correspond to Facies C lenses (i.e. are Early to Middle Pleistocene features). Magnetic palaeobarrier systems trending south‐southwest in the inner shelf and onshore beneath the Gippsland Lakes are orientated 15° different to the modern Ninety Mile Beach barrier trend. Offshore, they correlate stratigraphically to progradation packages of Facies B. Analysis of bore data in the adjacent onshore Gippsland Lakes suggests that a Pliocene barrier sequence 100–120 m below surface is overlain by fluvial sand‐gravel and lacustrine mud facies. The ferruginous sandstone beds resemble offshore Facies C, and are located where magnetic palaeoriver channel systems occur, implying Early to Middle Pleistocene ages. Presence of the estuarine bivalve Anadara trapezia in the upper lacustrine mud facies suggests that the Gippsland Lakes/Ninety Mile Beach‐type barriers developed over the past 0.2 million years. Further inland, magnetic river channels that cut across present‐day uplifted structures, such as the Baragwanath Anticline, suggest that onshore Gippsland uplift continued into the Middle Pleistocene.  相似文献   

State of the Society address     

Prof.  Jocelyn Bell Burnell FRS 《Astronomy& Geophysics》2003,44(4):4.34-4.36

Jocelyn Bell Burnell looks back over her first year as President of the Royal Astronomical Society.  相似文献