Facies-Dependent Occurrence of Shrinkage Cracks in the Glauconitic Sandstone, Semri Group, Vindhyan Supergroup-Reference-Cited by-同舟云学术

Facies-Dependent Occurrence of Shrinkage Cracks in the Glauconitic Sandstone, Semri Group, Vindhyan Supergroup

Published:2013-07-10 Issue:4 Volume:83 Page:389-395
ISSN:0369-8203
Container-title:Proceedings of the National Academy of Sciences, India Section A: Physical Sciences
language:en
Short-container-title:Proc. Natl. Acad. Sci., India, Sect. A Phys. Sci.

Author:

Singh B. P.,Mohan K.,Singh C. K.

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy

Link

http://link.springer.com/content/pdf/10.1007/s40010-013-0088-2.pdf

Reference37 articles.

1. Auden JB (1933) Vindhyan sedimentation in Son Valley, Mirzapur district. Mem Geol Surv India 62:141–250

2. Singh RM (1968) A study of the Glauconitic bed near Salkhan, district Mirzapur, U. P. Bull Geochem Soc India 3:24–31

3. Kumar S (1978) On the Kheinjua Formation of Semri Group, Lower Vindhyan, Newari area, Mirzapur district, UP. Proc Indian Nat Sci Acad 44A:144–154

4. Srivastava RN (1981) Significance of the grain size parameters in the Glauconitic sandstone of Semri Group in parts of Mirzapur district, U.P. In: Proceeding of the symposium on Vindhyans of Central India, GSI Misc Publications, 50, pp 175–180

5. Srivastava BN, Rana MS, Verma NK (1983) Geology and hydrocarbon prospects of the Vindhyan basin. Petrol Asia J 6:179–189

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Seismic origin of the soft‐sediment deformation structures in the upper Palaeo‐Mesoproterozoic Semri Group, Vindhyan Supergroup, Central India;Geological Journal;2020-06-02

2. Petrological study of the early Mesoproterozoic Glauconitic Sandstone and Olive Shale members from the Semri Group, Vindhyan Supergroup in Central India: Implications to input from intrabasinal felsic volcanic source and glauconitization;Geological Journal;2017-07-19