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Journal ArticleDOI

Petrography and metamorphism of the lower Gondwana (Permian) coal of Rangit Valley, eastern Himalays, India

T.K. Ghosh
- 01 Sep 1997 - 
- Vol. 33, Iss: 4, pp 351-368
TLDR
A triangular outlier of coal-bearing lower Gondwana rocks comprises a tectonic window within the Precambrian metamorphic terrain of the Rangit Valley, in the eastern Himalays of India as discussed by the authors.
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This article is published in International Journal of Coal Geology.The article was published on 1997-09-01. It has received 11 citations till now. The article focuses on the topics: Coal & Coal mining.

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Citations
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Journal ArticleDOI

Coal weathering and laboratory (artificial) coal oxidation

TL;DR: In this article, the effect of coal weathering and laboratory (artificial) oxidation on the microscopic appearance of coal, its microstructure as well as coal optical properties is discussed.
Journal ArticleDOI

Effect of igneous intrusive on coal microconstituents: Study from an Indian Gondwana coalfield

TL;DR: Petrological and palynological analyses of coals from two bore-holes, intruded by an igneous body (dolerite dyke), reveal characteristic changes due to thermal alteration.
Journal ArticleDOI

Petrographic and Raman spectroscopic characterization of coal from Himalayan fold-thrust belts of Sikkim, India

TL;DR: In this article, the optical anisotropy, optical sign, textural heterogeneity and deformational features of the maceral grains along with the Raman spectral characteristics of the seven coal samples collected from the Himalayan fold-thrust belts of Sikkim State, India.
Journal ArticleDOI

Spectral manifestations of coal metamorphism: Insights from coal microstructural framework

TL;DR: In this article, the microstructural framework of coals from the Raniganj and the Jharia Basins as well as from the Himalayan fold-thrust belts of Sikkim, India, by vitrinite reflectance, Raman spectroscopy, Fourier transform infrared, and X-ray photoelectron spectrographs was investigated.
Journal ArticleDOI

Organic matter type, origin and thermal maturity of Paleozoic, Mesozoic and Cenozoic successions of the New Siberian Islands, eastern Russian Arctic

TL;DR: In this article, a detailed characterisation of organic matter type and origin as well as determination of thermal maturity have been carried out on siliciclastic and carbonate sedimentary samples from Paleozoic, Mesozoic and Cenozoic outcrops of the New Siberian Islands, eastern Russian Arctic.
References
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Journal ArticleDOI

Melting on Fault Planes During Large Earthquakes

TL;DR: In this paper, it is shown that the temperature on the fault plane can reach the melting temperature for short periods if the slip is sufficiently large and the displacement required to produce melting depends on the magnitude of the regional stress and also on the friction stress.
Book

Organic maturation studies and fossil fuel exploration

J. Brooks
TL;DR: The main aim of Organic Maturation Studies and Fossil Fuel Exploration is to provide a platform for current research, developments, applications and discussion on organic maturation of sedimentary organic matter presented against the ever increasing requirements of petroleum exploration as discussed by the authors.
Journal ArticleDOI

Heating during thrust faulting in the rocky mountains: friction or fiction?

TL;DR: In this article, the authors measured the levels of organic maturation below and within shear zones of thrust faults in the Rocky Mountains and revealed no general thermal metamorphism that can be attributed to faulting, with the exception of very localized areas.
Journal ArticleDOI

Optical anisotropy of coals as an indicator of tectonic deformation, Broad Top Coal Field, Pennsylvania

TL;DR: The anisotropic reflectance fabric of coal is used as a finite strain marker in the structural analysis of deformed strata in the Broad Top Coal Field of central Pennsylvania.
Journal ArticleDOI

Radiometric dating of time of thrusting in the disturbed belt of Montana

TL;DR: The radiometric dating of the emplacement of the thrust plates by the K-Ar method has been studied in this paper, with ages ranging from 72 to 56 m.p.y.
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