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HYDROCHEMICAL STUDY IN THE PENCH VALLEY COAL MINE AREA, MADHYA PRADESH

Ullah, Mohammad Irfan (1995)

The area under study is a part of Pench Valley Coalfields and lies in Chhindwara district of Madhya Pradesh, India. The geographic co-ordinates of the region are 22°10'-15' latitudes and 78°40'-50' longitudes, a small ...

GEOMORPHOLOGICAL AND SEISMOTECTONIC EVALUATION OF THE REGION AROUND AGRA

Jindal, Anil Kumar (1995)

The Ganga basin is bounded by the Himalaya in the north and the Peninsular shield in the south. The northward thrusting of the Indian Plate has caused complex processes of intraplate deformation and reactivation of ...

GEOMORPHOLOGICAL AND PEDOLOGICAL EVOLUTION OF PARTS OF LOWER GANGETIC PLAINS IN WEST BENGAL

Singh, Lalan Prasad (1995)

The Lower Gangetic Plains form one of the most extensive fluvio-deltaic plains of the world. Quaternary climatic and sea level changes and tectonics have influenced significantly the development of landforms and soils ...

ACRITARCH BIOSTRATIGRAPHY OF THE ORDOVICIANSILURIAN SEQUENCE ALONG SUMNA-RIMKHIM SECTION, TETHYAN GARHWAL HIMALAYA, CHAMOLI DISTRICT, UTTAR PRADESH

Sinha, Hareshwar Narain (1995)

Rocks of the Lower Paleozoic marine sequence occur in the Tethyan Zone of the Himalaya with exposures in Kashmir, Spiti, (Himachal Pradesh) and Kumaon-Garhwal (Uttar Pradesh) regions of India. Although, these sediments ...

STUDY OF CRUSTAL AND UPPER MANTLE STRUCTURE ALONG SELECTED PATHS IN IRAN USING SURFACE WAVE DISPERSION

Kamalian, Nasrollam (1994)

Seismological studies in Iran have been motivated by the need to reduce earthquake hazards. A significant event in this regard was the setting up of three WWSSN stations at Tabriz, Shiraz, and Mashhad. We investigate ...

STRONG MOTION MODELLING OF RUPTURE PLANE ALONG AN IDENTIFIED PROBABLE CAUSATIVE FAULT

Joshi, Anand (1994)

Earthquakes are the most disastrous of all natural phenomenon. In this century alone, over five million lives have been lost due to earthquakes and they have been responsible for loss of property of over one hundred and ...

SEISMOLOGICAL STUDIES OF THE NW HIMALAYA BASED ON EARTHQUAKE DATA RECORDED IN THE GARHWAL HIMALAYA

Kumar, Sushil (1994)

This thesis is based on analysis of seismological data recorded with portable seismograph arrays operated during 1984-86 in the Garhwal segment ofthe northwest Himalaya. Thearrays were operated to monitor the local small ...

ON RUPTURE ZONES AND GEODYNAMIC PROCESSES OF GREAT EARTHQUAKES ALONG THE HIMALAYAN CONVERGENT PLATE MARGIN

Gahalaut, Vineet Kumar (1994)

This thesis is a compilation of six distinct yet complementary studies of great and moderate earthquakes along the Himalayan convergent plate margin. In the first study the extant largely qualitative evidence for ground ...

HYDROGEOLOGICAL STUDIES IN THE SOUTHEASTERN COASTAL TRACTS OF KUTCH WITH SPECIAL REFERENCE TO QUALITY OF GROUNDWATER

Bhatt, Kiran (1994)

The low lands of coastal Saurashtra and Kutch in Gujarat (India) have remained a part of the arid belt since at least Pleistocene time. Kutch is extremely susceptible to droughts and water scarcity conditions. The deficit ...

HYDROGEOLOGICAL INVESTIGATIONS OF THE DECCAN TERRAIN OF THE KOYNA SUB-BASIN, INDIA

Naik, Pradeep Kumar (1994)

The western margin of the Indian Peninsula is characterised by hilly terrain, known as Western Ghats (hills). The Koyna sub-basin (a part of Krishna River basin) is located east of the main ridge, locally called the ...

GEOMORPHOLOGICAL AND PEDOLOGICAL EVOLUTION OF PARTS OF BANGLADESH PLAINS

Hossain, MD. Shohrab (1994)

The Lower-Ganges-Brahmaputra-Meghna river system occupies most of Bangladesh and forms one of the world's largest fluvio-deltaic plains. Neotectonism and Worldwise Quaternary palaeoclimatic and sea level changes have ...

CRUSTAL STRUCTURE OF INDIA AND ADJOINING REGIONS USING RAYLEIGH WAVE DISPERSION

chauhan, P. K. S. (1994)

Among the different methods which have been used to deduce crustal structure from seismic observations, the use of surface wave dispersion holds a prominent place. This method has been used since early 1950's. The ...

HYDROCHEMICAL STUDIES IN UPPER HINDON BASIN, DISTT. SAHARANPUR, U.P., INDIA

Seth, Ashok Kumar (1993)

There is an increasing awareness for the maintenance of water quality especially in urban areas, while attempting to locate new and sizeable sources of water. The quality of natural waters has been affected by man through ...

COLLISION TECTONICS : METAMORPHIC AND GEOCHRONOLOGICAL CONSTRAINTS FROM PARTS OF HIMACHAL PRADESH, NW-HIMALAYA

Singh, Sandeep (1993)

The Himalaya is located on the seismically-active northern margin of the Indian Plate, and provides an unique opportunity to investigate collisionrelated geodynamic processes of a young orogenic belt during the ...

TERRAIN STUDIES FOR SLOPE INSTABILITY IN PARTS OF TEHRI DISTRICT, GARHWAL HIMALAYA, U.P., INDIA

Tabatabae, Saeid Hashemi (1992)

Himalaya is the youngest mountain range in the world. They owe their origin to the collision of Indian Plate with the Eurasian plate. With the continual subduction of Indian Plate, the Himalaya is still rising, thus, ...

PETROLEUM SOURCE ROCK STUDIES OF THE NON-MARINE BARAKAR SEDIMENTS, JHARIA, BIHAR, INDIA

Shahzeidy, Bahram Alizadeh (1992)

Commercial generation of petroleum, till recent years was thought mainly to be of marine origin. However, with the findings of substantial quantities of petroleum generated in the nonmarine sediments, from many parts ...

METAMORPHIC EVOLUTION OF THE HIGHER HIMALAYAN CRYSTALUNE, ZANSKAR, JAMMU AND KASHMIR

Asokan, A. (1992)

The Himalaya is a composite mountain be1t of the Trans- Himalayan batholith in north, followed successively in the south by the Indus-Tsangpo Suture Zone (ITSZ), Tethyan Sedimentary Zone (TSZ), Higher Himalayan Crystalline ...

A HOLOCENE SOIL-CHRONOASSOCIATION OF THE GANGETIC PLAINS BETWEEN RAMGANGA AND RAPTI RIVERS

Srivastava, Pankaj (1992)

Fourteen soil-geomorphic units have been delineated from the Gangetic plains between the Ramganga and Rapti rivers. The units delineated are based on remote sensing studies and field checks. One additional unit immediately ...

STRUCTURAL GEOMETRY AND STRAIN PATTERNS OF THE COLLISION ZONE, ZANSKAR, NW-HIMALAYA

Patel, Ramesh Chandra (1991)

The Himalayan Arc has been considered as archetype example of large-scale continental convergence caused by the subduction of the Tethyan Oceanic Crust and subsequent collision of the Indian Plate against the Eurasian ...

SEDIMENTOLOGICAL STUDIES OF THE INDUS SUTURE ZONE ROCKS, LADAKH, NW-HIMALAYA, INDIA, WITH SPECIAL REFERENCE TO THEIR SOURCE ROCK EVALUATION FOR PETROLEUM

Moezabadi, Mohammad Karamati (1991)

The Indus Suture Zone is a major crustal lineament between Himalayan range and Tibet. It runs for about 2500 km from Hindukush Mountain of Afghanistan to the Mishmi Hills of Assam in India. This important tectonic belt ...

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