TMMOBABSTRACT: i Die von A. C Houlsby vorgeschlagene Methode verwendet man bei den Staudaemmen für die auswertung von Probe-Injektionen diese Methode umfasst die errechmmg der Lugeon Werte, ihre Auswertung, Berechnung und Auswaehlung der für alle fünf Versuche, die unter steigenden und sinkenden drück durchgeführt sind, In diesem Vortrag wird versucht die beim Fırat - Gölköy Staudamm für Probe Injektion unter Druck durchgeführten Wasser - Versuche nach der von Houlsby vorgeschlagenen Methode auszuwerten, die Lugeon Verte zu bestimmen und nach der Ergebnissen die passenden Permeabilitaat zahlen zu waehlen, datmi werden noch die Faktoren von Permiae bilitat werte untersucht,
ÖZ: In the area of study, Paleozoic, Mesozoio, and Tertiary fonnations are present in the form of exotic blocks. Magmatic activity is widespread throughout the area and represented by volcanic rocks of tertiary age. Balya ore deposits are placed in the contact zone of dacite and limestone blocks and they can also be observed in the joints of the limestone formation. In the research of the ore deposits which are closely related to tectonic activity, 40 to 80 m spaced drill holes are necessary in works associated with drilling. Tectonic and field studies give the impression that ore potential of Balya area & quite high,
ABSTRACT: This new type of diagram is called a vector diagram because it is based on vectoral dimensions. In the beds of the Demirözü and Köse area south west of Bayburt nine formations have been discriminated. Only two formations, Sırataşlar and Kızılyar have been used in drawing the rose (Kg. 3 and 4), contour (Fig, 5) and vector (Fig. 6) diagrams. In order to draw a vector diagram, first concentric circles that have the radii r/9, 2r/9,... nr/n and r/4, 2r/4...nr/n are drawn. Then the East-West and North-South axes are added and the adequate dip degrés and percentage are written on the East-West axis. The details of this drawing are illustrated in Fig. 6. Afterwards the vectors of the average dipandpercentage are calculated and are put in to their places (like in a1..a5 and c1...c5) the average dip and percentage are shown bysolid and broken lines on the effect lines Predominant strikes can be found by adding tha two percentage vectors that are on the same line but in converse direction. As is known, predominant strikes are perpendicular to the dipvectors (a1c1-a5c5). Vector diagrams are more accurate and easier to use than others. The main advantage of vector diagram is that it is possible to read boththe average dips and their strikes directly from only one diagram. Finally, with vector diagram it is not necessary to make extensive explanations of the tectonic positions of formations in geological theses and reports.