AAPG Bulletin, V. 90, No. 2 (February 2006), P. 193-208.

Copyright copy2006. The American Association of Petroleum Geologists.
All rights reserved.
Di AAPG bulletin bulan Februari 06 ini, ada artikel seperti yg kita
diskusikan bulan lalu yaitu ttg fracture reservoirs.
Dalam paper ini juga disebutkan ada hubungan "scale-independency"
ketidak bergantungnya fracture dengan skala (ukuran). Ini salah satu
prediksi fracture reservoir dengan sample core yg mungkin bisa
dikembangkan dengan fracture yg diketemukan dalam seismic.
Kalau masih kurang jelas bisa menghubungi authornya lewat imilnya.

Hef e nais riding ...

RDP
======================= start quote =====

A scale-independent approach to fracture intensity and average spacing
measurement
Orlando J. Ortega,1 Randall A. Marrett,2 Stephen E. Laubach3

1Shell International Exploration and Production, 200 North Dairy
Ashford, Houston, Texas 77079; [EMAIL PROTECTED]

2Department of Geological Sciences, John A. and Katherine G. Jackson
School of Geosciences, University of Texas at Austin, Austin, Texas
78712-1101

3Bureau of Economic Geology, John A. and Katherine G. Jackson School
of Geosciences, University of Texas at Austin, Austin, Texas
78713-8924; [EMAIL PROTECTED]
ABSTRACT

Fracture intensity, the number of fractures per unit length along a
sample line, is an important attribute of fracture systems that can be
problematic to establish in the subsurface. Lack of adequate
constraints on fracture intensity may limit the economic exploitation
of fractured reservoirs because intensity describes the abundance of
fractures potentially available for fluid flow and the probability of
encountering fractures in a borehole. Traditional methods of
fracture-intensity measurement are inadequate because they ignore the
wide spectrum of fracture sizes found in many fracture systems and the
consequent scale dependence of fracture intensity. An alternative
approach makes use of fracture-size distributions, which allow more
meaningful comparisons between different locations and allow
microfractures in subsurface samples to be used for fracture-intensity
measurement. Comparisons are more meaningful because sampling
artifacts can be recognized and avoided, and because common thresholds
of fracture size can be enforced for counting in different locations.
Additionally, quantification of the fracture-size distribution
provides a mechanism for evaluation of uncertainties. Estimates of
fracture intensity using this approach for two carbonate beds in the
Sierra Madre Oriental, Mexico, illustrate how size-cognizant
measurements cast new light on widely accepted interpretation of
geologic controls of fracture intensity.

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