Gravity-driven sedimentation on the northwestern continental slope in the South China Sea: Results from high-resolution seismic data and piston cores     

T. Lüdmann 《中国海洋湖沼学报》1999,17(2):155-169

mODUCnONGravityflowsedimentationonthenorthwsterncontinentalsl0PeoftheSOuthChinaSea(SCS)are0fgreatinterestfromthescientificandengineeringP0intofview-Th0roughknOWedgofcontinentalsloPepmeessesanddepositionfeatUresispreregUisiteforhydID-carbenexploraion0fdeepwaerandforprotectionofoffhoredrineeopneeringstrUcbes(PlaifonnsandpiPelines)againstnaedhed.ManykindsofmassmovmentPIDCess-eswerefoUndtobeactiveonthen0rthernSCS(Damuth,l979;l98O).High-freqUency(3.5ffo)echo-chaIaCterInaPPingisawell…  相似文献   

Coupled finite‐element simulation of injection well testing in unconsolidated oil sands reservoir     

Bin Xu  Ron C.K. Wong 《国际地质力学数值与分析法杂志》2013,37(18):3131-3149

This paper presents a finite‐element (FE) model for simulating injection well testing in unconsolidated oil sands reservoir. In injection well testing, the bottom‐hole pressure (BHP) is monitored during the injection and shut‐in period. The flow characteristics of a reservoir can be determined from transient BHP data using conventional reservoir or well‐testing analysis. However, conventional reservoir or well‐testing analysis does not consider geomechanics coupling effects. This simplified assumption has limitations when applied to unconsolidated (uncemented) oil sands reservoirs because oil sands deform and dilate subjected to pressure variation. In addition, hydraulic fracturing may occur in unconsolidated oil sands when high water injection rate is used. This research is motivated in numerical modeling of injection well testing in unconsolidated oil sands reservoir considering the geomechanics coupling effects including hydraulic fracturing. To simulate the strong anisotropy in mechanical and hydraulic behaviour of unconsolidated oil sands induced by fluid injection in injection well testing, a nonlinear stress‐dependent poro‐elasto‐plastic constitutive model together with a strain‐induced anisotropic permeability model are formulated and implemented into a 3D FE simulator. The 3D FE model is used to history match the BHP response measured from an injection well in an oil sands reservoir. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

»Late Jurassic« petroleum geology of the Dutch Central North Sea Graben     

Th. E. Wong  Th. H. M. van Doorn  B. M. Schroot 《International Journal of Earth Sciences》1989,78(1):319-336

The Callovian to Ryazanian (late Middle Jurassic to earliest Cretaceous; here referred to as »Late Jurassic«) sediments of the Dutch Central North Sea Graben, comprising the Central Graben and Scruff Groups, form several potential reservoirs. Source rocks are present within both these groups and the Carboniferous and Late Triassic-Early Jurassic.The structural development of the area is illustrated by a number of cross-sections. A structural subdivision has been made into platform, intermediate platform, outer graben, and inner graben. The complex history of rifting, wrench-faulting, halokinesis, and structural inversion strongly influenced the palaeogeography and ensuing sandstone developments. A few selected burial-history plots are presented as examples of the relationship between the structural subdivision and the hydrocarbon potential of the area.

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Zusammenfassung Die Sedimente des Callov bis zum Ryazan (oberer Mitteljura bis unterste Kreide, hier als »Oberjura« bezeichnet) des zentralen niederländischen Nordsee-Grabens, der den Zentralgraben und die Scruff-Gruppe umfaßt, stellen mehrere potentielle Erdölspeichergesteine dar. In jeder dieser beiden Gruppen sowie im Karbon und von der Obertrias bis zur Unterkreide existieren Speichergesteine.Die strukturelle Entwicklung des Gebietes wird anhand mehrere Profile veranschaulicht. Außerdem schien eine Untergliederuntg in Plattform, Zwischenplattform, äußerer sowie innerer Graben sinnvoll. Die komplexe Entwicklungsgeschichte, die durch Riftingphasen, Wrench-Tektonik, Halokinese und Strukturinversion bestimmt wurde, hat die Paläogeographie und die resultierende Sandsteinbildung intensiv beeinflußt. Eine Anzahl ausgewählter Darstellungen der Geschichte der Sedimentüberlagerung dienen als Beispiele für den Zusammenhang zwischen den strukturell bestimmten Untergruppen und dem Kohlenwasserstoffpotential des Untersuchungsgebietes.

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Résumé Dans le secteur néerlandais du Graben Central de la Mer du Nord, plusieurs réservoirs potentiels sont constitués par les sédiments calloviens à ryazaniens (ensemble allant du sommet du Jurassique moyen au Crétacé inférieur et désigné ici par «Late Jurassic»). Ces sédiments comprennent le groupe du Graben central et le groupe de Scruff. Des rochesmères existent dans chacun de ces deux groupes ainsi que dans le Carbonifère et dans la série Trias terminal-Eojurassique.La constitution structurale de cette région est illustrée par une série de coupes. On distingue, au point de vue structural: une plate-forme, une plate-forme intermédiaire, un graben externe et un graben interne. L'histoire géologique complexe, avec ses processus de rifting, de décrochement, d'halokinèse et d'inversion structurale, s'est répercutèe de manière significative sur la paléogéographie et, par voie de conséquence, sur l'extension des faciès arénacés. Quelques reconstitutions de l'histoire sédimentaire sont présentées à titre d'exemple de manière à illustrer la relation entre les unités structurales et le potentiel en hydrocarbure de la région.

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, Scruff, -. Callov Ryazan/ ; « »/. - / . . , , . , , . , .

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Observations of mine seismicity in the eastern Wasatch Plateau,Utah, U.S.A.: A possible case of implosional failure     

Ivan G. Wong  James R. Humphrey  Janet A. Adams  Walter J. Silva 《Pure and Applied Geophysics》1989,129(3-4):369-405

In the summer of 1984, a three-dimensional, high-resolution microearthquake network was operated in the vicinity of two coal mines beneath Gentry Mountain in the eastern Wasatch Plateau, Utah. During a six-week period, approximately 3,000 seismic events were observed of which the majority were impulsive, higher frequency (>10 Hz), short duration (<2–3 sec) events probably associated with the caving of the roof from a longwall operation. In contrast, 234 of the largest located events appeared to occur predominantlybeneath the mines to a depth of 2 to 3 km consistent with previous studies. The magnitudes of these events ranged from less thanM _c 0 to 1.6. In addition to the unusual depths of these latter events, an anomalous aspect displayed by the events was an apparent dilatational focal mechanism suggesting a non-double-couple, possibly implosional source. Implosional events have been observed in other studies of mine seismicity; however, the generally inadequate instrumental coverage of the focal sphere has cast some doubt on the validity of such mechanisms. Previously suggested source mechanisms for such implosional events have included tensional failure through strata collapse, and a shear-implosional displacement mechanism. Shear failure must be involved in the failure process of the Gentry Mountain implosional events as evidenced by well-defined shear waves in the observed seismograms. Simultaneous monitoring in the East Mountain coal mining area to the south by the University of Utah revealed typical shear failure events mixed with implosional events. The observed double-couple, reverse focal mechanisms at East Mountain were similar to mechanisms determined in previous studies and a composite focal mechanism determined in this study for a sequence outside the mining areas. This suggested that the shear events within the mining areas are being influenced by the regional tectonic stress field. Thus in addition to the seismic events associated with caving of the roof from the longwall operation, there appear to be at least two other types of mining-induced seismic events occurring in the eastern Wasatch Plateau, both submine in origin: (1) events characterized by apparent non-double-couple possibly implosional focal mechanisms and well-defined shear waves; and (2) shear events, which are indistinguishable from tectonic earthquakes and may be considered mining triggered earthquakes. The small mining-induced stress changes that occur beyond a few hundred meters from the mine workings suggest both types of seismic events are occurring on critically stressed, pre-existing zones of weakness. Topography, overburden, method of mining, and mine configuration also appear to be significant factors influencing the occurrence of the implosional submine events.  相似文献   

PHYSICAL GEOGRAPHY IN SOUTHEAST ASIA: PAST THEMES, CURRENT STATUS AND FUTURE TRENDS     

Avijit Gupta  M.A.  Ph.D.  P.P. Wong  M.A.  Ph.D. 《Singapore journal of tropical geography》1994,14(2):252-264

Our knowledge regarding the physical geography of Southeast Asia is incomplete to a surprising extent. This paper reviews the past research, describes the ongoing work, and attempts to identify the future trends. Coverage of such a large area, even for the last 25 years, requires study of publications in several languages and coping with literature which is not easily available. Therefore certain topics. which are prominent in current research and likely to remain so in the future were chosen and reviewed in detail. Such topics include studies related to active plate margin features; the Pleistocene in Southeast Asia; erosion and sedimentation rates; rainforest; river systems; karst in Southeast Asia; coastal geomorphology; and the urban environment. Environmental studies are rapidly gaining importance chiefly because of (a) the destruction of the natural vegetation and the associated loss of biodiversity and (b) the growing problems due to accelerated erosion and sedimentation This trend is likely to continue with accelerated destruction of forests, development of coastal areas, and urbanization of the landscape The direction of research in physical geography of Southeast Asia has been determined by a combination of individual research interest, governmental priorities, and international expectations  相似文献   

FORTY YEARS OF PHYSICAL GEOGRAPHY IN THE JOURNAL     

P.P. Wong  M.A.  Ph.D.  Avijit Gupta  M.A.  Ph.D. 《Singapore journal of tropical geography》1994,14(2):295-309

Up to June 1993, 207 articles on physical geography have been published in the Malayan Journal of Tropical Geography (MJTG) (1953–57), Journal of Tropical Geography (JTG) (1958–79) and the Singapore Journal of Tropical Geography (SJTG) (1980–93). These articles are examined initially in terms of their sub-fields (Biogeography, Climatology, Geomorphology, Hydrology, and Soils), area of focus (the tropics, Africa, America, East Asia, South Asia, Southeast Asia excluding Malaysia and Singapore, Malaysia, Singapore, and Southwest Pacific) and the area of origin of the authors. The more significant papers in the sub-fields are indicated. Various factors influencing the contributions to the Journal and some insights on the contributions of local staff (Singapore and Malaysia) are also given. The significance of the Journal as an avenue for local and foreign authors and for papers on physical geography in the tropics is briefly evaluated.  相似文献   

INDUSTRIAL FORESTRY     

T. M. Wong 《Singapore journal of tropical geography》1993,13(1):63-74

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UPb zircon and rutile chronology of Archean greenstone formation and gold mineralization in the Val d'Or region, Quebec     

L. Wong  D.W. Davis  T.E. Krogh  F. Robert 《Earth and Planetary Science Letters》1991,104(2-4)

UPb geochronology provides an absolute time framework for the evolution of the Sigma gold deposit and surrounding rocks at Val d'Or, southern Abitibi subprovince. The Bourlamaque batholith, the largest pluton in the area, gives a 2699.8 ± 1.0 Ma UPb zircon age. This pluton cuts the Val d'Or Formation which hosts the mineralization. A UPb zircon age of 2704.9 ± 1.1 Ma on a felsic volcanic rock, the Colombière “rhyolite”, 13 km east of the mine dates that formation. The gold-bearing quartz vein system at Sigma is hosted by andesites and two generations of porphyry intrusions, all metamorphosed to the greenschist facies. The oldest porphyry (“porphyritic diorite”) shows the same deformation as the volcanic rocks, and has a 2703.7 ± 2.5 Ma UPb zircon age. The porphyritic diorite and volcanic rocks are cut by feldspar-porphyry dykes which post-date regional folding and have a 2694.0 ± 2.2 Ma UPb zircon age.Regional greenschist metamorphism has been dated directly, with a UPb date of 2684 ± 7 Ma on rutile in the Colombière “rhyolite”. The mineralization and hydrothermal alteration in the mine are superimposed on the metamorphic minerals. Hydrothermal rutile, from an alteration halo around the veins in andesite, has a 2599 ± 9 Ma UPb age. Textural evidence clearly indicates that the wall-rock alteration and vein filling are contemporaneous, and hence the vein system and gold mineralization appear to have developed at least 80 m.y. after the formation and metamorphism of host greenstones.  相似文献   

The toxicity of marine sediments in Victoria Harbour, Hong Kong   总被引：4，自引：0，他引：4  

Y. S. Wong  N. F. Y. Tam  P. S. Lau  X. Z. Xue 《Marine pollution bulletin》1995,31(4-12):464-470

When the toxicity of marine sediment in Hong Kong was evaluated, it was found that the seven sediments collected within Victoria Harbour were severely contaminated with heavy metals, at concentrations many times higher than those in sediments collected from outside the harbour. The highest metal content was recorded in site VS14 (located near the airport runway and the industrialized area), with copper, zinc, lead and chromium values of 3789, 610, 138 and 601 mg kg⁻¹ dry wt, respectively. This site also had the greatest alkaline phosphatase activities (15 fluorescent intensity unit g⁻¹ wet wt), the largest number of total coliforms (910 CFU g⁻¹ wet wt) and sulphate-reducing bacteria (8.5 × 10⁴ cells g⁻¹ wet wt), implying that site VS14 was also contaminated with organic matter and nutrients. Sediment bioassays, Microtox and algal tests, demonstrated that sediment elutriates obtained from site VS14 were of greatest toxicity. The EC₁₀ value in Microtox tests was 17% elutriate, and the 96-h IC₅₀ values using Skeletonema costatum and Dunaliella tertiolecta were 40 and 79% elutriate, respectively. No toxic effects were found in sediment samples collected from the control site outside Victoria Harbour. Significant correlations were found between the results of the algal toxicity test (using S. costatum) and the coliform count and metal content of the sediments. The Microtox test was less sensitive than the algal bioassay, and no sediment elutriate, even from the site mostly contaminated by heavy metals, caused more than 50% inhibition of the light-emitting activity of the bacteria. In this study, S. costatum (the diatom) provided a more sensitive and reliable test species than D. tertiolecta (the flagellate) in differentiating the toxicity of marine sediments.  相似文献   

Diffraction of plane sh waves in a half-space     

A. H. Shah  K. C. Wong  S. K. Datta 《地震工程与结构动力学》1982,10(4):519-528

Scattering of antiplane shear waves (SH) in two dimensions by surface and near-surface defects in a homogeneous, isotropic elastic semi-infinite medium has been studied. Attention has been focused here in the range of medium to long wavelengths. A combined finite element and analytical technique has been used to study the problems of scattering by semi-circular and triangular canyons. The results for the former case are compared with the known exact solution and those for the latter case are compared with some available approximate solutions. Finally a problem of multiple scattering by a triangular canyon and a nearby circular tunnel is studied. Numerical results are presented showing the effects of multiple scattering and different angles of incidence. These results are of interest in earthquake engineering.  相似文献