Giriş Topical Term

Kullanılan kayıt sayısı: 1

001 - CONTROL NUMBER

• control field: 101261

003 - CONTROL NUMBER IDENTIFIER

• control field: DLC

005 - DATE AND TIME OF LATEST TRANSACTION

• control field: 20160523074413.0

008 - FIXED-LENGTH DATA ELEMENTS

• fixed length control field: 050309i| anannbabn |a ana

010 ## - LIBRARY OF CONGRESS CONTROL NUMBER

• LC control number: sh 85047491

040 ## - CATALOGING SOURCE

• Original cataloging agency: DLC
• Transcribing agency: DLC
• Modifying agency: DLC
• Modifying agency: WaU
• Modifying agency: DLC

053 #0 - LC CLASSIFICATION NUMBER

• Classification number element--single number or beginning number of span: QE606
• Classification number element--ending number of span: QE606.5

150 ## - HEADING--TOPICAL TERM

• Topical term or geographic name entry element: Faults (Geology)

450 ## - SEE FROM TRACING--TOPICAL TERM

• Topical term or geographic name entry element: Fault lines (Geology)

450 ## - SEE FROM TRACING--TOPICAL TERM

• Topical term or geographic name entry element: Faulting (Geology)

450 ## - SEE FROM TRACING--TOPICAL TERM

• Topical term or geographic name entry element: Geological faults

450 ## - SEE FROM TRACING--TOPICAL TERM

• Topical term or geographic name entry element: Lines, Fault (Geology)

550 ## - SEE ALSO FROM TRACING--TOPICAL TERM

• Control subfield: g
• Topical term or geographic name entry element: Geology, Structural

670 ## - SOURCE DATA FOUND

• Source citation: LC database, Mar. 9, 205
• Information found: (title: geological faults)

670 ## - SOURCE DATA FOUND

• Source citation: Forsmark site investigation : searching for evidence of late- or postglacial faulting in the Forsmark region, 2005:
• Information found: abstr. ("Major faulting" is defined as dislocations in the order of several metres along faults several kilometres long)

670 ## - SOURCE DATA FOUND

• Source citation: Wikipedia, Aug. 26, 2009
• Information found: (Fault (geology); "In geology, a fault or fault line is a planar fracture in rock in which the rock on one side of the fracture has moved with respect to the rock on the other side. All faults have a measurable thickness, made up of deformed rock that is characteristic of the level in the crust where the faulting happened, the rock types affected by the fault and the presence and nature of any mineralising fluids.")