印支地块思茅地区始新统磁倾角偏低现象及其构造意义     

安纯志  杨振宇  仝亚博  李晨皓  王恒  高亮  韩志锐  徐颖超 《吉林大学学报(地球科学版)》2017,47(2)

对印支地块思茅地区始新世陆相红层进行古地磁研究,获得勐伴剖面特征剩磁方向为Ds=118.2°,Is=22.1°,k=31.6,α95=10.9°;勐腊剖面特征剩磁方向为Ds=47.6°,Is=22.8°,k=20.2,α95=5.9°。其特征剩磁方向与前人研究结果基本一致。利用Hodych等的磁倾角校正方法得到校正磁倾角为28.4°±4.3°,对前人的数据重新进行E/I统计得到的校正磁倾角值为30.7°,置信区间为[25.4°,35.9°],两种不同方法得到了较一致的结果,思茅地区的古近纪磁倾角显示了一定程度的偏低。E/I磁倾角偏低检验方法在应用时存在一定的局限性,变形微弱地层的古地磁学数据适合进行E/I磁倾角偏低校正,以避免倾伏褶皱或差异性旋转变形作用对E/I磁倾角偏低校正的影响。Hodych等提出的磁倾角校正方法是现今比较可靠的磁倾角校正方法。结合前人印支地块的古地磁研究成果,本次研究结果表明印支地块思茅地区自始新世以来相对于华南板块向南滑移量约500km。  相似文献   

粤西雷州半岛地区1∶5万区域地质调查成果与主要进展     

李响  张宗言  张楗钰  刘祥 《华南地质与矿产》2019,35(3):293-305

在粤西雷州半岛地区完成的1∶5万区域地质调查,以最新的国际地层表为指南,建立并完善了调查区多重地层划分与对比系统。采用岩性-岩相-火山机构三重填图方法,查明了调查区内火山岩的岩石特征及产出分布特征,详细划分了火山岩相类型及其组合,划分了火山活动旋回,系统总结了各喷发期火山岩的岩石学、地球化学特征,并探讨了火山岩的成因;综合遥感、路线地质调查、物探与钻探等多种方法,基本查明了坡头-海康港隐伏断裂(四会—吴川断裂的南延北支)及火山构造等的展布特征,初步建立了调查区构造格架。开展地质灾害调查,编制了雷州半岛中西部地质灾害分布与易发区图;开展河头镇和唐家镇幅土壤环境专项调查,绘制了土壤质量地球化学等级图,综合评定良好级以上土壤655km^2,圈定富硒土壤510km^2;探索和总结了适用于雷州半岛覆盖区的地质填图方法。  相似文献   

BOOK REVIEWS     

《The Professional geographer》1984,36(1):106-142

Book Reviewed in this article: Development and Environment in Peninsular Malaysia . S. Robert Aiken, Colin H. Leigh, Thomas R. Leinbach, Michael R. Moss. The Rural-Urban Fringe: Canadian Perspectives . Ken B. Beesley and Lorne H. Russwurm, eds. Women and Development . Lourdes Benería, ed. The Border that Joins: Mexican Migrants and U.S. Responsibility . Peter G. Brown and Henry Shue, eds. Cities of the World: World Regional Urban Development . Stanley D. Brunn and Jack L. Williams, eds. Time Resources, Society, and Ecology: On the Capacity for Human Interaction in Space and Time (Vol. I, Preindustrial Societies). Tommy Carlstein. Urban Geography . David Clark. Spanish City Planning in North America . Dora P. Crouch, Daniel J. Garr, and Axel I. Mundigo. Not On Our Street: Community Attitudes to Mental Health Care . M. J. Dear and S. M. Taylor Unequal growth: Urban and Regional Employment Change in the U.K. Stephen Fothergill and Graham Gudgin. Agricultural Land in an Urban Society . Owen J. Furuseth and John T. Pierce. The Petroleum Industry in Oil-Importing Developing Countries . Fariborz Ghadar. Historical Understanding in Geography, An Idealist Approach . Leonard Guelke. Regional Planning in Europe . R. Hudson and J. R. Lewis, eds. Remote Sensing for Resource Management . Chris J. Johannsen and James L. Sanders, eds. Geography and The State . R. J. Johnston. Texas Graveyards: a Cultural Legacy . Tlrry G. Jordan. The Politics of Location: An Introduction . Andrew Kirby. A Social Geography of the City . David Ley. Energy and the Future . Douglas MacLean and Peter Brown, eds. The Natural Environment of Newfoundland Past and Present . A. G. Macpherson and J. B. Macpherson, eds. Tourism: Economic, Physical and Social Impacts . Alister Mathieson and Geoffrey Wall. Railroads and Land Grant Policy: A Study in Government Intervention . Lloyd J. Mercer. Progress in Rural Geography . Michael Pacione, ed. Progress in Urban Geography . Michael Pacione, ed. Models of Spatial Inequality: Settlement Patterns in Historical Archaeology . Robert Paynter. Natural Hazard Risk Assessment and Public Policy, Anticipating the Unexpected . William J. Petak and Arthur A. Atkisson. The Nature of Geomorphology . Alistair F. Pitty. Regional Conflict and National Policy . Kent A. Price Women and Spatial Change: Learning Resources for Social Science Courses . Arlene C. Rengert and Janice J. Monk, eds. Urban and Regional Analysis for Development Planning . Richard Rhoda. Rivers: Form and Process in Alluvial Channels . Keith Richards. This Remarkable Continent: An Atlas of United States and Canadian Society and Culture . John F. Rooney, Jr., Wilbur Zelinsky, and Dean R. Louder, gen. eds. The Origins of Open-Field Agriculture . Trevor Rowley, ed. Residential Location Determinants of the Older Population . Gundars Rudzitis. Borderland Sourcebook: A Guide to the Literature on Northern Mexico and the American Southwest . Ellwyn R. Stoddard, Richard L. Nostrand, and Jonathan P. West, eds. Arctic and Antarctic . David Sugden. Tall Timbers Ecology and Management Conference, February 22–24, 1979, Proceedings No. 16 . Graphic Communication and Design in Contemporary Cartography (Progress in Contemporary Cartography , Vol. II). D. R. Fraser Taylor, ed. Living with Energy Shortfall: A Future for American Towns and Cities . Jon Van Til. The United States: Habitation of Hope . J. Wreford Watson. Air Photo Interpretation for Archaeologists . D. R. Wilson. Urban and Rural Change in West Germany . Trevor Wild, ed. Population and Resources . Harry Robinson.  相似文献   

Ring complexes in the Peninsular Ranges Batholith, Mexico and the USA: magma plumbing systems in the middle and upper crust   总被引：1，自引：0，他引：1  

S. E. Johnson  K. L. Schmidt  M. C. Tate 《Lithos》2002,61(3-4):187-208

Subvolcanic ring complexes are unusual in that they preserve a rapidly frozen record of intrusive events. This sequential history is generally lost or complicated in plutons owing to mixing and mingling in a dynamic state. Thus, subvolcanic ring complexes are more like erupted rocks in their preservation of instantaneous events, but the self-contained nature of the complexes allows detailed structural and chemical work to be conducted in environments where the relative timing between individual magmatic events is commonly well preserved.

We suggest that development of subvolcanic ring complexes in the western Peninsular Ranges Batholith (PRB) involved the following three-stage generalized sequence: (1) fracturing of the roof above a buoyant or overpressured magma chamber, which resulted in moderately inward-dipping conical fractures that locally hosted cone sheets; (2) subsequent loss of magma from the chamber, combined with degassing of the melt, which facilitated collapse of the roof along near-vertical ring faults that locally hosted ring dikes; and (3) resurgence of the chamber, and/or intrusion of a broadly cogenetic nested pluton, which locally destroyed evidence for the earlier history of the system. This sequence has been repeated twice in one of the ring complexes that we have identified, which resulted in nested intrusive centers.

Calderas, subvolcanic ring complexes and plutons may represent progressively deeper sections through linked magma plumbing systems, and the systematic occurrences of these features in the western PRB are consistent with progressively deeper along-strike exposures of the batholith from south to north over a distance greater than 250 km.

In addition to subvolcanic complexes in the western PRB, deeper crustal levels exposed in the transition zone between eastern and western parts of the batholith preserve ring complexes emplaced at depths of up to 18 km. Occurrence of these deeper-level complexes suggests either that caldera subsidence can extend to mid-crustal levels or that other processes can produce ring complexes.  相似文献   

Superposed folding in the Honakere arm of the Chitradurga-Karighatta schist belt in the Dharwar tectonic province,southern India,and its bearing on the Sargur-Dharwar relation     

K. Naha  A. Rai Choudhuri  V. Ranjan  R. Srinivasan 《Journal of Earth System Science》1995,104(3):327-347

The supracrustal enclave within the Peninsular Gneiss in the Honakere arm of the Chitradurga-Karighatta belt comprises tremolite-chlorite schists within which occur two bands of quartzite coalescing east of Jakkanahalli(12°39′N; 76°41′E), with an amphibolite band in the core. Very tight to isoclinal mesoscopic folds on compositional bands cut across in the hinge zones by an axial planar schistosity, and the nearly orthogonal relation between compositional bands and this schistosity at the termination of the tremolite-chlorite schist band near Javanahalli, points to the presence of a hinge of a large-scale, isoclinal early fold (F₁). That the map pattern, with an NNE-plunging upright antiform and a complementary synform of macroscopic scale, traces folds 'er generation (F ₂),is proved by the varying attitude of both compositional bands (S₀) and axial pranar schistosity (S ₁), which are effectively parallel in a major part of the area. A crenulation cleavage (S ₂) has developed parallel to the axial planes of theF ₂ folds at places. TheF ₂ folds range usually from open to rarely isoclinal style, with theF ₁ andF ₂ axes nearly parallel. Evidence of type 3 fold interference is also provided by the map pattern of a quartzite band in the Borikoppalu area to the north, coupled with younging directions from current bedding andS ₀ -S ₁ inter-relation. Although statistically theF ₁ andF ₂ linear structures have the same orientation, detailed studies of outcrops and hand specimens indicate that the two may make as high an angle as 90°. Usually, in these instances, theF ₁ lineations are unreliable around theF ₂ axes, implying that theF ₂ folding was by flexural slip. In zones with very tight to almost isoclinalF ₂ folding, however, buckling attendant with flattening has caused a spread of theF ₁ lineations almost in a plane. Initial divergence in orientation of theF ₁ lineations due to extreme flattening duringF ₁ folding has also resulted in a variation in the angle between theF ₁ andF ₂lineations in some instances. Upright later folding (F₃) with nearly E-W strike of axial planes has led to warps on schistosity, plunge reversals of theF ₁ andF ₂ axes, and increase in the angle between theF ₁ andF ₂ lineations at some places. Large-scale mapping in the Borikoppalu sector, where the supposed Sargur rocks with ENE ‘trend’ abut against the N-‘trending’ rocks of the Dharwar Supergroup, shows a continuity of rock formations and structures across the hinge of a large-scaleF ₂ fold. This observation renders the notion, that there is an angular unconformity here between the rocks of the Sargur Group and the Dharwar Supergroup, untenable.  相似文献   

PALEOMAGNETIC EVIDENCE FOR THE RELATIVE MOTION BETWEEN THE SOUTH CHINA BLOCK AND INDOCHINA BLOCK   总被引：1，自引：0，他引：1       下载免费PDF全文

Lin Jin-lu 《地震地质》1988,10(3):7

The Mesozoic paleomagnetic pole positions from the Indochina block and South China block are not consistent with each other in that the formers are displaced with respect to the latters westward in longitude and southward in latitude. The displacement is here interpreted as to be related to the India-Eurasia collision in such a way that after the collision the Indochina block was rotated clockwise by 8° about the Assam syntaxis, followed by an eastward translation of the South China bl..  相似文献   

Soil carbon dioxide and weathering potentials in tropical karst terrain,peninsular Malaysia: A preliminary model     

J. Crowther 《地球表面变化过程与地形》1984,9(5):397-407

CO₂ concentrations at depths of 15,30, and 50 cm were determined over a one-year period in six karst soils in the Malay peninsula. Evidence suggests that the highest single CO₂ value (MAXCO₂, per cent) recorded at each site/depth provides the best estimate of conditions during groundwater recharge events. Soil depth (cm) and bulk density (BDEN) are the best predictors of MAXCO₂, with the equation loglo(MAXCO₂) = 1·146 (BDEN) + 0·00698 (DEPTH) - 1·227 accounting for 86 per cent of the variation. This equation is used to model MAXCO₂ at seven, more remote sites. Soil throughflow patterns and groundwater recharge points are estimated from slope pantometer and soil depth surveys in order to assess the CO₂ concentration with which soil waters ultimately equilibrate before entering the limestone. Limestone weathering seems to be predominantly of the open system type, the overall mean MAXCO₂ of 1·65 per cent corresponding with a weathering potential of 167 ppm CaCO₃. Weathering potentials vary markedly, ranging from 62–82 ppm on rocky hilltops to more than 280 ppm on certain tower karst footslopes in Selangor and the Kinta Valley and on moderate hillslopes developed in impure limestones in the Boundary Range.  相似文献   

Origin of Ca in South Indian calcretes developed on metamorphic rocks     

N. Durand  S.M. Ahmad  B. Hamelin  Y. Gunnell  P. Curmi 《Journal of Geochemical Exploration》2006,88(1-3):275

Calcrete profiles developed on Precambrian silicate rocks in south peninsular India are studied and compared in terms of mineralogical, chemical and isotopic composition. The aim of this study is to determine the origin of calcium and the processes governing the development of a minor economic deposit in different geomorphic settings. The investigation integrates observations from an outcrop to a microfabric scale and reveals that the origin of calcium is local and linked with the weathering of the minerals of the surrounding rocks. The CaCO₃ precipitation occurs after vertical and lateral translocation in the slope system.  相似文献   

Estimation of seismic spectral acceleration in Peninsular India   总被引：6，自引：0，他引：6  

S. T. G. Raghu Kanth  R. N. Iyengar 《Journal of Earth System Science》2007,116(3):199-214

Peninsular India (PI), which lies south of 24°N latitude, has experienced several devastating earthquakes in the past. However, very few strong motion records are available for developing attenuation relations for ground acceleration, required by engineers to arrive at rational design response spectra for construction sites and cities in PI. Based on a well-known seismological model, the present paper statistically simulates ground motion in PI to arrive at an empirical relation for estimating 5% damped response spectra, as a function of magnitude and source to site distance, covering bedrock and soil conditions. The standard error in the proposed relationship is reported as a function of the frequency, for further use of the results in probabilistic seismic hazard analysis.  相似文献   

Zinc and Copper Concentrations in Two Species of Intertidal Crabs from the Middle of the West Coast of Peninsular Malaysia     

Ahmad Ismail  Chee Kong Yap 《湿地科学》2009,7(3):218-229

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