This  geological excursion to Poland has realized as a result of the scientific cooperation and exchange between INSTITUTE OF GEOLOGY AND PALEONTOLOGY, UNIVERSITY OF TUBINGEN, and INSTITUTE OF GEOLOGY,  UNIVERSITY OF WARSAW.The program of  the excursion includes presentation of  the structures strictly comparable  in our two  countries,  as  exemplified by some Paleozoic and Mesozoic sequences of  the Holy Cross Mountains,  as well as of  the structures different  in their type of  development,  as exemplified by the Neogeae sequence of   the Fore-Carpathian Depression. To make better opportunities for studying  the selected sections,   this  very   FIELD-GUIDE is presented to our best colleagues and friends.

Investment decisions are critical part of a company’s success, and capital budgeting is a central topic of financial management. However, in contrast to other strategic decisions in business, decisions on capital projects are decentralized, from corporate to divisions, divisions to operations, from operations to departments. Engineers at various levels within the organization who make a capital proposal are contributing to the strategic success of the organization. This book will assist engineers to contribute strategically to the organization, so that they can contribute to the success of their company and can make a success of their careers.<...>

Faults and their deeper-level equivalents, shear zones are localized regions of higher strain which effectively accommodate differential movement in the Earth's crust and mantle during deformation of the lithosphere. Shear zones may be more precisely defined as approximately tabular regions of concentrated deformation and flow across which adjacent relatively undeformed rock units are offset.

The Masjed Daghi mineralization is located 30 km southeast of Jolfa city at the bank of Araxes River, northwest Iran. This area is situated in the AlborzAzarbaijan structural zone of Iran. The most widespread rocks in the mineralization area are andesite and trachyandesite, while there are rock units of latite tuff, andesitic agglomerate, and hornblende porphyry basalt in eastern hills and Eocene flysch in the southern part of the area. Several intrusive bodies are present in the study area, from which the dominant intrusive rock hosting the mineralization is diorite porphyry.