The sub-Himalayan zone of the Himalaya is bounded by the Main Boundary Thrust (MBT) in the northern side and by the Himalayan Frontal Thrust (HFT) in the southern side. HFT is the youngest major tectonic boundary of the Himalaya, separating the Siwalik Hills from the Indo-Gangetic plains. The HFT and Piedmont fault make the densely populated foothill region vulnerable to seismicity. A morphotectonic

The Chalk hills of Salem complex also called Salem mafic and ultramafic complex (SMUC), occurs in northern part of Cauvery suture zone (CSZ), southern granulite terrane (SGT), India with the lithological sequence of ultramafic cumulates, mafic intrusions of gabbros and amphibolites with quartzo-feldspathic veins and ultrapotassic dykes. Recently the complex has been described as Neoproterozoic Alaskan-type

The present paper describes the abundant and very well preserved ichnotaxon complex Hillichnus agrioensis, as established by four different morphological levels of exposures. Associated trace-fossils such as Jamesonichnites heinbergi and Ancorichnus ancorichnus are also being reported from the Hettangian to Bajocian Thaiat Member of Lathi Formation of Jaisalmer basin, western Rajasthan, India. The

The Simlipal complex in eastern India is an elliptical structure with diameter of ca. 50 km coinciding with an elliptical region of high gravity. It overlies the Archaean basement of the Singhbhum craton and has a ring structure characterized by complex series of concentric ridges with inward dipping slopes. Quartz clasts in melt-breccias from the complex display diagnostic shock metamorphic features

Kuttanad area is part of the western coastal plains in Kerala characterized by a thick pile of Tertiary sediments underlying the Recent alluvium. The evolution of aquifer systems in these sediments are closely related to the geological history of the area and the groundwater in the Tertiary aquifer system was evolved during various marine transgressions and regressions. Chemical processes such as leaching

Parameters like aquifer depth, aquifer replenishment rate, aquifer medium, soil medium, percolation medium, and the coefficient of permeability are considered during the preparation of a groundwater vulnerability diagram. The analytic hierarchy process is used for evaluation, and expert scoring is used to analyze and establish the judgment matrix, and then new weights have been computed for each DRASTIC

The coastland of Saurashtra is represented by several estuaries, islands and cliffs. Taxonomy and seasonal distribution of the recent benthic foraminifera along the coastal tracts of the Saurashtra region have been documented. Surface sediments were collected from the fifteen stations of this coast in both pre and post-monsoon. A total of 35 calcareous wall structure bearing species are identified

The regionally extensive Ramu-Markham-Fault-Zone (RMFZ) in Papua-New-Guinea (PNG) passes through the seismically-active hinterland of the Bismarck subduction zone in SW-Pacific. The seismicity map for 400km segment of RMFZ shows that higher magnitude earthquakes mainly originate in four spatial clusters (I–IV), asymmetrically disposed from in-land to offshore on either side of RMFZ. The cluster III

In the year 2013, the Northwestern Himalaya witnessed an extreme hydrological event that severely affected the upper Ganga Basin. The unexpected high sediment mobilisation in the basin affected the human population, infrastructure, and ecology in several reaches of the Ganga river and its tributaries. In an exceedingly affected reach, the Kedarnath valley, a considerable sediment volume (∼26243 × 104

The objective of the study was to find the significant impact of season on the outdoor gamma dose rate including statistical analysis. Outdoor gamma dose rates were studied for 52 locations of the Balod district, Chhattisgarh, India, in summer and winter. Statistical analysis confirmed that there was no significant difference in dose rate between summer and winter. Geology of the area was the most

The rise of groundwater level in slope due to intense rainfall is one of the factors that can trigger slope failure. The groundwater level rise causes increase in the pore water pressure thus reducing the shear resistance of the soil. The purpose of this study is to present a groundwater level evaluation system in response to daily rainfall for slope stability forecasting. The system consists of three

During blasting operations for fluorite in the mining area of the Amba Dongar, numerous xenoliths of different rock types were brought to the surface from time to time in the last several years. The present study is based on the uncovered fenitized gneissic xenoliths in sövite exposed in the mining area. With the aid of detailed petrography and BSE images it is documented that protolith gneiss has

The occurrence and relative stability of metamorphic allanite and monazite in metapelites of the Greater Himalayan Sequence (GHS) in the Dhauliganga valley, Garhwal Himalaya have been studied. The GHS is marked by kyanite grade metamorphism in the lower and middle structural levels and sillimanite grade metamorphism in the upper structural level. The occurrence of allanite is restricted to the lower

Murshidabad is an alluvial terrain in the Gangetic plains of West Bengal. Water is mainly stored in the pore spaces of the formation and thus the yield is quite good from the aquifers of this region. But the suitability of this water for human use not only depends on quantity of groundwater available but also to a great extent on the chemical quality of groundwater. which has direct effect on human

This study reconstructs the pre-impact orientation of impact-generated µm-sized microstructures. The approach is illustrated using a sample from the basement dolerites of the Lockne impact structure, Sweden. Under the polarised light microscope, the microstructure appears as alternating augite-plagioclase wedges. The top-view of the microstructure is presented in the polished thin-section using light

The Ongole coastal dunefield (OCD) is about 20 km long and 2.5 to 3 km wide, and is located to the east of Ongole town between the mouth of the Paleru river in the south and a small creek in the north. Much of the dunefield lies 3–5 m above sea level with some large dune ridges reaching 10–12 m. The area landward of the dune field consists of an extensive marsh. Optically stimulated luminescence (OSL)

In Cambay basin (India) a thick sedimentary sequence exits consisting of shales. This sequence is known as Cambay Shale Formation (both younger and older). In the present investigation 57Fe Mössbauer spectroscopy study was carried on samples of Cambay Shale Formation. These samples are collected from various depth interval from well UBER#2. Results thus obtained are also compared with the Mössbauer

The present study generates a glacial lake inventory of Arunachal Pradesh, Eastern Himalaya, India using Landsat 8 Operational Land Imager (OLI) images (2016-2018). The study reveals that there are in total 1532 (> 0.001 km2) glacial lakes, covering an area of 93.7 km2. Glacier erosion lakes are the most dominant type with 1268 glacial lakes (82.8%) and an area of 76.8 km2 (∼82%). About 50% of the

Downstream changes in channel morphology and its flow were investigated over a monsoon dominated Dwarkeswar river from the western part of West Bengal. The basin has developed over the Proterozoic Granite Gneiss Complex to recent Holocene alluvium, forming three distinctive geomorphological regions of the basin e.g., dissected plateau, plate-fringe and alluvial plain area. Sixty cross-sections along

The abundance of garnet — hornblende pair in a wide range of rocks primarily from upper green schist to granulite facies has made it one of the most widely used pairs for estimation of temperature at which once rocks equilibrated. Several models of garnet- hornblende thermometer have been formulated by a number of researchers in last four decades. In this contribution, four thermometers: Graham & Powell

In the present study, the tectono-geomorphic attributes of the northern part of the Cambay basin, Western India, which has recently witnessed a surge in seismic activity has been investigated. The anomalies in the drainage network (morphometry) along with the sedimentological character of the drainages with OSL chronology was used to unravel the abrupt aggradation and incision processes during the

This study was undertaken to quantify the naturally occurring arsenic in the groundwater and chemical body burden caused by its ingestion at some villages of Fatehabad district, Haryana, India. The arsenic levels in groundwater were quantified by hydride generation atomic absorption spectrometry (HG-AAS). Arsenic concentration in the groundwater was found to be in the range of <0.05 to 4.53 µg L−1

Palaeo-geographical conditions control the sedimentological and hydrological heterogeneity within the upper aquitard and late Pleistocene aquifers beneath Kolkata. Such complexity at Bowbazar was unmapped prior to the Tunnel Boring Machine (TBM) of East-West metro project which hit the local aquifer at 14 m depth. This led to development of cracks in tens of buildings due to land subsidence; few of

The Higher Himalayan Crystallines (HHC) in the Siyom river section of eastern Arunachal Himalaya, display top-to- ESE compressional ductile shear from Pene to Menchuka. In this part of the Himalayan Metamorphic Belt (HMB), the base of the Main Central Thrust (MCT) is the southern boundary of the ductile shear fabrics in HHC. Across the MCT, a significant break in the grade of metamorphism is observed

The present work attempts to analyze the slope stability of road section along the national highway NH-1D from Sonamarg to Kargil in the erstwhile J&K, India. The rugged and treacherous terrain in this region is prone to frequent slope failures taking heavy toll of life, property and inconveniences to commuters due to disruption of vehicular movement. For slope study analysis twenty facets were chosen

Heavy mineral assemblages of sedimentary units are used as an essential provenance constraint. The sedimentary successions of the southern Assam and Siwalik foreland basins were analyzed for their heavy mineral suits and provenance determination. Heavy minerals were identified using the petrological microscope, X-ray Diffraction (XRD) and Electron Probe Micro Analyzer (EPMA) analyses. The study demonstrates

The groundwater resources of basaltic terrains in peninsular India are decreasing rapidly, due to indiscriminate extraction without considering the recharge capabilities of an aquifer. The main focus of the present study is to develop a good perceptive of the groundwater recharge capabilities in basaltic terrains for long term groundwater sustainability. In the present study 3D aquifer solid model

Groundwater flow modeling is an important tool for understanding and computing hydrology and water availability of an aquifer zone. However, an accurate representation of boundaries and their initial conditions are vital for simulation of the groundwater flow phenomena. In this study, efforts have been made to develop a GIS based methodology for estimating flux across boundaries of the study area using

In the present work, the morphometric and morphotectonic analysis of the Pahuj basin catchment of the Bundelkhand region of Central India was carried by using remote sensing and GIS techniques. The drainage map, Digital Elevation Model (DEM), density, contour, aspect, and other thematic maps were extracted from ASTER-DEM (30m resolution) data by using geographical information system (GIS) tool. Five

Himalayan region is seismically one of the most active continental regions. It experienced at least 4 M ∼ 8 earthquakes during an active phase from 1897 to 1952. However, no such earthquake has occurred since 1952. Detailed investigations have revealed that the region is currently in a seismic quiescence phase, and enough strains have been accumulated to source several M ∼ 8 earthquakes. However, when

The Himalayan range, being a complex terrain, is highly prone to slope instability in many parts because of the natural conditions and human interference. In the present study, road cut slope stability assessment has been carried out along Chamba-Bharmour Section (Chamba District, Himachal Pradesh) along Chakki (Pathankot, Punjab) - Bharmour (Chamba, Himachal Pradesh). The cut slopes with the potential

The stratigraphic sequence exposed in Wandhaya area comprises of marine clastic sediments of Mesozoic, which includes M-III and M-IV of Jumara Formation, Lower Member of Jhuran Formation and Upper Member of Bhuj Formation. Lithofacies erected from the study area are Shale Facies (SF), Oolitic Limestone Facies (OLF), Intercalated Shale Siltstone Facies (ISSF) and Massive Sandstone Facies (MSF). SF is

In this paper, Anisotropy of Magnetic Susceptibility (AMS) data from the rocks of Almora crystalline in the vicinity of Rameshwar is presented. The study integrates field, microstructural and Anisotropy of Magnetic Susceptibility (AMS) studies. Field foliation strike shows NW-SE orientation with moderate to high dip in rocks of Almora Crystalline, whereas near North Almora Thrust rocks of Almora Crystalline

The accurate determination of factor of safety is important to find out the stability of slopes. Out of the many factors which are responsible for slope failure in hilly areas continuous rainfall, particularly, is one of the major important factor responsible for triggering landslide. Slope is an exposed ground surface that stands at an angle with the horizontal. In this study, a part of the hill of

Water scarcity has become a major problem especially in arid and semi-arid regions due to insufficient rainfall throughout the globe. This has led in serious search for groundwater resources. Kanavi Halla Sub Basin (KHSB) of Ghataprabha River basin drained by Ghataprabha River, Belagavi District of Karnataka state in India has been considered for present study. Electrical resistivity survey was carried

A majority of the existing groundwater potential studies in the literature lack adequate validation. In developing countries, it is attributed to many reasons including-poor/limited data on water yield, sparse spatial and temporal data on wells, lack of data protocol/sharing, a weak ground water governance structure such as disparate agencies, lack of registration/georeferencing of irrigation wells

Siliciclastic sediment succession of the Bairenkonda Formation of the Proterozoic Cuddapah Supergroup overlies the granite-gneiss of the east Dharwar craton along a nonconformity in the Tirumala hills. Basin fill sediments are now classified in ascending order into three lithofacies assemblages namely; lower cross-stratified sandstone (CSS); middle sand-dominated heterolithic (MH) and upper shale-dominated

In the Precambrian Singhbhum stratigraphy, some enigmatic aspects exist as regards to Dangoaposi and Jagannathpur lavas. The existing enigma embodies locational aspects of these lavas, structural characteristics, stratigraphic position, and geochemical affinities. Based on recent field studies by the authors and knowledge acquired from existing literature, a possible solution has been proposed in the

Major hydrochemical ionic concentrations in groundwater has been analyzed during dry and wet periods (pre-monsoon and post-monsoon periods, respectively) in a semi-arid Sanganer block, Jaipur district, Rajasthan, India. The standard methods were utilized for evaluating its appropriateness for irrigation and drinking uses. Results indicate that groundwater is moderately alkaline and predominantly Ca-Na-HCO3-type

Slope instability is a big challenge for the population in mountainous regions. It poses a threat to life, economy, and infrastructure. For the safety of people, various prevention and precautions are taken and hence many scientific studies are going on. In the present study, the stability of the Karmi landslides zone, Bageshwar, Uttarakhand, India is assessed. Karmi village lies quite close to the

Manganese mineralization in the Precambrian Gangpur Group of rocks in Sundargarh district of Odisha occur as pockets or small ore bodies associated with metapelites and metapsamites. Different varieties of hypogene metamorphic manganese minerals belonging to Mn-oxides, Mn-carbonates, Mn-silicates, Mn-titanates have been reported from this Group. Although the Mn-bearing rocks and the Mn-ores host several

Clinopyroxene relict magmatic phases in Neoarchean Mangikhuta volcanics are described in detail in terms of their geochemistry for the first time, and their petrogenetic insights obtained. EPMA study indicates their restricted compositional range. Elemental variation diagrams show progressive variation of Al, Ca, Si, Fe+3, Ti, Cr, Aly and Aly/Alz, Ti/Al, Fe+2/Fe+3 elemental ratios with fractionation

The REE-2 is a carbonatite sample with rare earth elements provided from a Canadian mining company and distributed by Canadian Certified Reference Materials (CCRM), Canada. The reference material was provided to participate in the testing process (round-robin) and CSIR-NGRI, Hyderabad, state of the art analytical technique Energy Dispersive X-ray fluorescence (EDXRF) also contributed to the development

Groundwater (GW) contamination due to urbanization, industrialization and agriculture is a major environmental problem in India. The present case study aims to estimate the vulnerability of the aquifer with the help of GIS based DRASTIC method. A micro watershed, characterized by Granites and Gondwana Formation in the vicinity of Koradi, 15 km from Nagpur in Central India has been considered. The DRASTIC

Hydrogeochemical evaluation and assessment of groundwater quality was carried for selected areas of Bishnupur district of Manipur to ensure its suitability for drinking and irrigational uses. Twenty physico-chemical parameters of groundwater samples from thirty-one spatially distributed areas were assesed including major geogenic contaminants such as Fe3+, As3+ and F− to ensure public health safety

Kanchankayi is located in the central part of the 55 km long Kurlagere-Gogi-Gundanahalli (KG) fault of Meso-Neoproterozoic Bhima basin of Southern India. Intensive integrated exploration in Kanchankayi has established a concealed, fracture-controlled, low-grade uranium deposit. Uranium mineralisation is mostly confined within the fractured limestone of Shahabad Formation and partly within fractured

This study investigates the geomorphic expression of tectonic control in Koyna-Warna shallow seismic region, lying on Deccan Flood Basalt in India, by examining longitudinal profiles and morphometric parameters by using Digital Elevation Model (DEM) and constrained field examinations. A total of 60 sub-catchments have been analyzed to comprehend the relative tectonic control in the study area. Sub-catchments

Long-term and short-term assessments of sediment yield from river basins are required in planning soil conservation measures, water storage in reservoirs and prediction of morphological responses in rivers. In present study, detailed quantification of land-use land-cover and climate variabilityin two contrasting subcatchments of Upper Tapi basin, India, are reported for period 1980–2010. The pattern

A common phenomenon associated with the alluvial river is its meandering action which leads to lateral migration and thus geomorphic hazards. Predicting and preventing this migration is both difficult and necessary. Barak river is one of the highly meandering rivers flowing through the alluvial plains of Assam, India. It is observed that there is a regular shifting of the river banks and development

Dharwar craton (DC), by far the largest geological domain in South Indian Shield, occupying about 0.5 million sq. km area, is well-studied terrain both for regional geoscientific aspects and as part of mineral exploration over several important blocks such as the greenstone belts, ultramafic complexes, granite-gneissic terrain and the Proterozoic sediments of Cuddapah basin. The re-look into regional

The coal formation of the Damodar basin is found in parts of the Indian states of West Bengal and Jharkhand. However, the potentiality of the coal formation and its presence across the basin are not equal. Both East Bokaro and West Bokaro are highly fertile and productive for high-quality coal. However, due to the lack of coal seams, no significant discoveries can be made between these two regions

Underground surge pool cavern for the storage and lifting of water is being constructed in the part of Telangana State of India. For better rock mass characterization and support design, 3D engineering geological mapping was carried for the heading portion of the surge pool. 3D geologic mapping of heading portion is very important for large underground cavern to know about the cavern behavior during

Roof bolt failures in the mine generally occur due to the poor identification of the weak rock layers and considered as a major concern for underground coal mines in terms of its productivity and safety. The triggering factor responsible for underground roof failure is the presence of weak bedding planes and various geological discontinuities. Geological disruptions present in the mine roof seriously

This paper gives an overview of the deep-water ventilation studies carried out over the world oceans using radiocarbon. There is a consensus that aged water mass existing in the abyssal ocean during the last glacial, dissipated during the Heinrich Stadial 1 (HS1; 17.5–14.7 ka) and the Younger Dryas (YD; 12.9–11.7 Ka, cold event) and hence ventilation increased. The data from the Arabian Sea is in agreement

As per the 2017 global reports, 63 million Indians are living in rural areas without access to the safe drinking source of water. Access to the safe drinking water was declared as a human right by the United Nations but remains a challenge for India. Due to increase in demand of water, 30% of urban and 90% of rural households completely depend on untreated surface or groundwater, which causes serious

The study integrates the morphometric analysis, lineament evaluation and fluvial geomorphology to investigate the morphotectonic setup of Sai basin. The Sai river basin forms an integral part of the central Ganga plain where the gentle slope is significantly controlled by intra-basinal tectonic activity. The fluvial setup of the Sai basin which comprises of vast old flood plains now is displayed as

The Papaghni sub-basin of the Cuddapah basin is an arcuate NW-SE trending intracratonic basin, stretching from Kurnool in the NW to Guvvalacheruvu in the SE, in southern peninsular India. Despite of large number of researches, an understanding of the evolution of the basin is still elusive. The sub-basin preserves records of repeated opening and closing of Paleoproterozoic rifts along the zone of NW-SE

Geochemical data (major and minor oxides, trace elements including REE, and Sr, Nd, Pb, and O isotopes) have been obtained on a number of flow sequences and plutonic and volcanic complexes of the DVP by numerous groups since the early 1970’s. Evaluation of these data has led to the classification of the basalts and other rock types, inferences on their mantle sources, parental magmas and the numerous

A comprehensive study of the manganese ore deposits of Banswara manganese belt (23°10′-23°20′N to 74°15′-74°25′E) in the Banswara district, Rajasthan, has shown a characteristic assemblage of manganese ore minerals. The manganese ore deposits are associated with Aravali phyllite, schist, quartzite and limestone, etc., and occur within a narrow linear belt trending NW-SE. These meta-sediments hosted

Landslides are the natural geomorphic processes that are essential for the landscape development. Loss of tremendous amount of life, natural resources as well as property has made this phenomenon a natural disaster. Number of researches have been done to understand this phenomenon and how to overcome this calamity with the aid of upcoming modern information services and technological advancements.