Srivastava,P., Sangode,S.J., Meshram,D.C., Gudadhe,S.S., Nagaraju,E., Kumar,A. and Venkateshwarlu,M.(2012): Paleoweathering and depositional conditions in the inter-flow sediment units (bole beds) of Deccan Volcanic Province, India: A mineral magnetic approach. Geoderma, 177-178, 90-109.

『インドのデカン火山州の流間堆積物ユニット(膠灰粘土層)における古風化と堆積条件:鉱物磁性からのアプローチ』


Abstract
 A total of 54 samples from thirteen different profiles of interflow sediment units occurring in the Deccan Volcanic Province (DVP, India) are studied using an integrated mineral magnetic and field documentation approach. The occurrence and distribution of ferri- and antiferromagnetic oxides associated with these sediments infer depositional conditions dominated by various detrital modes and recycling of baked sediments under limited authigenic environments. The baking of underlying sediments is conditioned by aqueous or dry nature of the substrate via-a(頭に`)-vis the viscosity of the overlying lava flow that can be identified by a combination of brown/red boles and compact/pahoehoe type flows. The presence of antiferromagnetic superparamagnetic (SP) fraction in the ‘red bole capped brown boles’ indicates the depth of baking to 〜20 cm; while the SP fraction also marks infilling, recycling and pigmentation in other occurrences of the red boles studied here.
 Overall, the mixed magnetic mineralogy and sediment characters depict frequent recycling and re-deposition by surface run-off, infiltration and ponding as the most common processes of bole bed formation in DVP governed by shallow basalts is frequently shown by the red and brown boles, while infilling into the interstices and cavities is common with green boles. The red boles are also characteristic of detrital mixing of oxidized/partially oxidized ferrimagnets, many times coated with pigmentary hematites. The present results envisage a great scope for the routine mineral magnetic studies (integrated with field observations) for rapid characterization of the extensively occurring bole bed horizons in the DVP and their study as analogs of Martian soils and sediments.

Keywords: Deccan Volcanic Province; Bole beds; Mineral magnetism; Paleoweathering』

1. Introduction
2. Study area and methods
 2.1. Experimental methods
3. Field description of individual bole bed profiles
 3.1. ZW profile
 3.2. DG-2
 3.3. DG-3
 3.4. DG-4
 3.5. Sus-1
 3.6. PG-1
 3.7. PG-2
 3.8. RH-1
 3.9. KJO-1
 3.10. RGB
 3.11. DGB/3
 3.12. KRB-1a
 3.13. AMT/GB
 3.14. Summary of the field characteristics
4. Mineral magnetic results
5. Profile wise interpretations
 5.1. Zindewadi profile (ZW)
 5.2. Dive Ghat (DG/2)
 5.3. Dive Ghat (DG/3)
 5.4. Dive Ghat (DG/4)
 5.5. SUS-1
 5.6. Pirangut (PG-1)
 5.7. Pirangut (PG-2)
 5.8. RH-1
 5.9. KJO-1
 5.10. RGB
 5.11. DGB/3
 5.12. KRB-1a
 5.13. AMT/GB
6. Genesis and distribution of magnetic minerals in the bole beds
7. Paleoweathering and depositional conditions of the bole beds formation
8. Conclusion
Acknowledgments
References


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