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Registros recuperados: 4
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Landscape response to progressive tectonic and climatic forcing in NW Borneo: Implications for geological and geomorphic controls on flood hazard ArchiMer
Menier, David; Mathew, Manoj; Pubellier, Manuel; Sapin, Francois; Delcaillau, Bernard; Siddiqui, Numair; Ramkumar, Mu.; Santosh, M..
Empirical models have simulated the consequences of uplift and orographic-precipitation on the evolution of orogens whereas the effects of these forcings on ridgelines and consequent topography of natural landscapes remain equivocal. Here we demonstrate the feedback of a terrestrial landscape in NW Borneo subject to uplift and precipitation gradient owing to orographic effect, and leading to less-predictable flooding and irreversible damages to life and property. Disequilibrium in a large catchment recording the lowest rainfall rates in Borneo, and adjacent drainage basins as determined through., a proxy for steady-state channel elevation, is shown to result in dynamic migration of water divide from the windward-side of the orogen towards the leeward-side...
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Ano: 2017 URL: https://archimer.ifremer.fr/doc/00638/75040/75697.pdf
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High resolution facies architecture and digital outcrop modeling of the Sandakan formation sandstone reservoir, Borneo: Implications for reservoir characterization and flow simulation ArchiMer
Siddiqui, Numair A.; Ramkumar, Mu.; Rahman, Abdul Hadi A.; Mathew, Manoj J.; Santosh, M.; Sum, Chow W.; Menier, David.
Advances in photogrammetry have eased the acquisition of high-resolution digital information from outcrops, enabling faster, non-destructive data capturing and improved reservoir modeling. Geocellularmodels for flow dynamics with in the virtual outcrop in siliciclastic deposits at different sets of sandstone facies architecture remain, however, a challenge. Digital maps of bedding, lithological contrast, spatial-temporal variations of bedding and permeability characteristics make it more easy to understand flow tortuosity in a particular architecture. An ability to precisely model these properties can improve reservoir characterization and flow modeling at different scales. Here we demonstrate the construction of realistic 2D sandstone facies based models...
Tipo: Text Palavras-chave: Siliciclastic sandstone facies; Connectivity; Heterogeneity; Digital outcrop model; Flow dynamics.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00637/74937/76048.pdf
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Early Cenozoic rapid flight enigma of the Indian subcontinent resolved: Roles of topographic top loading and subcrustal erosion ArchiMer
Ramkumar, Muthuvairavasamy; Menier, David; Mathew, Manoj; Santosh, M.; Siddiqui, Numair A..
Intrinsic magmatic processes are considered as critical operators of plate movements. Here we demonstrate the role of extrinsic processes consequent to intrinsic processes as a catalyst for anomalous rapid plate movement. The rapid and accelerated flight of the Indian subcontinent since Deccan volcanism until its collision with Eurasia remains as one of the geological conundrums. Data on seismic tomography, peninsular geomorphology and inferences on continuum of subcrustal structures are utilized to address this enigma. We propose geomorphic isostasy as the mechanism that has driven this fastest drift ever recorded in geological history. It was initiated by sudden instability after the Deccan volcanism and resultant extensive accumulation of lava pile over...
Tipo: Text Palavras-chave: Geomorphic isostasy; Mantle plume; Continental drift; Plate reorganization; India.
Ano: 2017 URL: https://archimer.ifremer.fr/doc/00638/75053/75674.pdf
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Structural controls on polyphase hydrothermal dolomitization in the Kinta Valley, Malaysia: Paragenesis and regional tectono-magmatism ArchiMer
Ramkumar, Mu; Siddiqui, Numair Ahmed; Mathew, Manoj; Sautter, Benjamin; Hui, Poon Xin; Nagarajan, R.; Breitfeld, H. Tim; Santosh, M.; Menier, David; Poppelreiter, Michael.
In the eastern side of the Malay Peninsula, thick successions of limestone formations preserve important records of the Mesozoic and Cenozoic tectonic events. Here we investigate the strata- and fracture-bound hydrothermal dolomites in the Palaeozoic carbonates of the Kinta Valley, western Peninsular Malaysia. Based on their textural and morphologic characteristics, structural relationships with the host rock, different facies types, and associations with hydrothermal calcite and low-grade metamorphic marble, we attempt to trace their polyphase origin and relationship with thereto-tectonic events of the region. A detailed evaluation of the nature of brecciation and crystallization of polyphase dolomites, dolomitic limestones, limestones and marble, under...
Tipo: Text Palavras-chave: Hydrothermal dolomite; Tectonics; Magmatism; Paragenesis; Structural evolution; Malaysia.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00637/74938/83485.pdf
Registros recuperados: 4
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