LABORATORY MEASUREMENT IN EXPLORATION BY IP METHOD IN ORDER TO DIFFERENTIATE MASSIVE FROM DISSEMINATED MINERALIZATION

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MIRZAEI S.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Journal of the Earth and Space Physics Year:2000 | Volume:26 | Issue:1 Page(s): 61-70

Download Full-Text

Persian Verion

View:

1,005

Download:

Cites:

Information Journal Paper

Title

LABORATORY MEASUREMENT IN EXPLORATION BY IP METHOD IN ORDER TO DIFFERENTIATE MASSIVE FROM DISSEMINATED MINERALIZATION

Author(s)

MIRZAEI S. | | Issue Writer Certificate

Keywords

ANOMALYQ4

APPARENT POLARIZABILITYQ4

MASSIVEQ4

DISSEMINATED AND IP PROCEDUREQ4

Abstract

Laboratory experiments have a specific significance in mining exploration to determine electrical properties of rock specially in the intended parameters in IP procedure. For the time being, IP geophysical procedure receives a specific significance in metallic ore deposits exploration. However, separation of IP anomalies of MASSIVE from disseminated mineralization according to the measured IP amounts with common procedures isn't possible. This research has been done on measurement of polarizability in the Taknar copper ore deposits. on the basis of laboratory experiment, polarizability has been measured in three normal directions (A, B, C), and then the mean APPARENT POLARIZABILITY in different time after cut off has been calculated. As a result of this operations, a model is presented on which by measuring APPARENT POLARIZABILITY and then their mean in two early and late time after cut off (e. g. one 0.5 and the other 17 seconds after electricity cut off and calculation of η̅17/η̅0.5 ratio) We can separate the anomalies of the mineralizations. The ratio specimens in MASSIVE mineralization are dramatically larger than disseminated mineralization. This result is used in mining exploration. It's necessary to state that the mean for APPARENT POLARIZABILITY in 0.5 second after electricity cut off for MASSIVE and disseminated mineralization have a relatively high and approximately near each other amounts and so if only 11 0.5 is measured, separation. Between the APPARENT POLARIZABILITY anomalies from the mineralization point of view is not possible.

Cites

No record.

References

No record.

Cite

APA: Copy

MIRZAEI, S.. (2000). LABORATORY MEASUREMENT IN EXPLORATION BY IP METHOD IN ORDER TO DIFFERENTIATE MASSIVE FROM DISSEMINATED MINERALIZATION. JOURNAL OF THE EARTH AND SPACE PHYSICS, 26(1), 61-70. SID. https://sid.ir/paper/80544/en

Vancouver: Copy

MIRZAEI S.. LABORATORY MEASUREMENT IN EXPLORATION BY IP METHOD IN ORDER TO DIFFERENTIATE MASSIVE FROM DISSEMINATED MINERALIZATION. JOURNAL OF THE EARTH AND SPACE PHYSICS[Internet]. 2000;26(1):61-70. Available from: https://sid.ir/paper/80544/en

IEEE: Copy

S. MIRZAEI, “LABORATORY MEASUREMENT IN EXPLORATION BY IP METHOD IN ORDER TO DIFFERENTIATE MASSIVE FROM DISSEMINATED MINERALIZATION,” JOURNAL OF THE EARTH AND SPACE PHYSICS, vol. 26, no. 1, pp. 61–70, 2000, [Online]. Available: https://sid.ir/paper/80544/en

Related Journal Papers