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Issue 01

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Effect of Salt Crystallization on the Building Stones Used in Konya,Central Turkey

VEYSEL ZEDEF; MURAT UNAL (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-12-20)
Eliminating Undesirable Compounds in Lubricant Oil by Clay

F. KHOJASTEH; N. EBADATI; M. NIKAZAR; Z. MYLANY; N. BEHZAD (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-12-20)
Contribution from Mafic Melt to the Zhireken PorphyryMo-Cu Deposit, Eastern Transbaikalia,Russia: Evidence fromMafic Microgranular Enclaves

ANITA; N. BERZINA; I.SOTNIKOV; VITALY (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-12-20)

Mafic microgranular enclaves (MME) were formed in felsic ore-bearing porphyries from the Zhireken por-phyry Mo-Cu deposit, eastern Transbaikalia, Russia. Porphyry rocks were emplaced during the Upper Jurassic. Most ofthe ...
Petrochemistry and Depositional Environment of Permian Coals ofBasundhara Block, Ib-Valley Coalfield, Orissa, India

R. K. SINGH; K. N. SINGH; S. K. DHANORIA; A. BHATT; A. DIXIT (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

This paper deals with the characteristics of coals of Basundhara block of Ib-valley. The aim of this study is toreconstruct the paleo-environment condition of coal formation. A large number of pillar coal samples from ...
Petrogenesis of Bir Madi Gabbro-Diorite and Tonalite-GranodioriteIntrusions in Southeastern Desert, Egypt: Implications forTectono-Magmatic Processes at the Neoproterozoic Shield

M. A. OBEID (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite Complex(GDC) and a Tonalite-Granodiorite Suite (TGrS). The GDC has a weak tonalitic to strong calc-alkaline character and ...
Petrochemical Characteristics and Age of Rare Metal (Ta-Nb)Mineralization in Precambrian Pegmatites,Komu, Nigeria

A. OLUGBENGA; G. OKUNLOLA; UDOUDO, B. OFONIME (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

The Precambrian pegmatites of Komu area intrude semi discordantly older rock types, such as biotite gneiss,amphibolites and pelitic schists. The pegmatites occur as near flat lying bodies. This study aims ...
Moho Discontinuity Depth Estimates for the Cameroon Volcanic Linefrom Gravity Data

MARCEL, C. T. JEAN; E. TABOD; DICOUM, MANGUELLE; P. N.NJANDJOCK (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

In this work, the Moho depth in a part of the Cameroon Volcanic Line (CVL) between the latitudes 3°30 ́ to6°33 ́N and the longitudes 8°50’ to 11°27’E, has been estimated covering two distinct regions: the Mount Cameroon ...
Drainage Characteristics of Tectonically Active Areas: An Examplefrom Rajasthan, India

SWATI JAIN; P. K. VERMA (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

The morphotectonic studies help in deciphering the role of tectonics and neotectonics in morphologicalevolution of drainage basins. On the basis of remote sensing technique, the relationship between ...
Volcanic Successions of the Jebal Remah Volcano, Northeast Jordan

AL-MALABEH, AHMAD (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

Jebal Remah volcano is one of huge but very poorly known tephra cones exposed on the basalt province ofHarra El-Jabban. Detailed investigations indicate that this volcano is topographically distinct and structurally ...
Pre and Post Earthquake Seismo-Tectonic Scenario of Hazara–Kashmir Terrain of Pakistan

TAHIRKHELI, R. A. KHAN (Karachi: Department of Geology, University of Karachi, Pakistan, 2010-01-20)

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