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Key stretching

Known as: Key strengthening, Key extension, Passphrase strengthening 
In cryptography, key stretching techniques are used to make a possibly weak key, typically a password or passphrase, more secure against a brute… 
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Related topics

Related topics

49 relations
.htpasswdArgon2BcryptBlock cipher

Broader (1)

Key management

Papers overview

Semantic Scholar uses AI to extract papers important to this topic.
Highly Cited
2017
Highly Cited
2017
The 2015 Plains Elevated Convection at Night Field Project
AbstractThe central Great Plains region in North America has a nocturnal maximum in warm-season precipitation. Much of this… 
Highly Cited
2011
Highly Cited
2011
FIRST EVIDENCE OF COEXISTING EIT WAVE AND CORONAL MORETON WAVE FROM SDO/AIA OBSERVATIONS
“EIT waves” are a globally propagating wavelike phenomenon. They were often interpreted as fast-mode magnetoacoustic waves in the… 
Highly Cited
2009
Highly Cited
2009
FPGA implementation of AES encryption and decryption
Advanced Encryption Standard (AES), a Federal Information Processing Standard (FIPS), is an approved cryptographic algorithm that… 
Highly Cited
2006
Highly Cited
2006
An Atomistic-to-Continuum Framework for Nonlinear Crystal Mechanics Based on Asymptotic Homogenization
Highly Cited
2005
Highly Cited
2005
Volcanic passive margins
Highly Cited
2000
Highly Cited
2000
Dynamics of weakly strain-hardening fluids in filament stretching devices
Highly Cited
1999
Highly Cited
1999
Persistent patterns in transient chaotic fluid mixing
Chaotic advection of a fluid can cause an initially inhomogeneous impurity (a passive scalar field) to develop complex spatial… 
Highly Cited
1993
Highly Cited
1993
Structure of the Dead Sea Pull-Apart Basin From Gravity Analyses
Analyses and modeling of gravity data in the Dead Sea pull-apart basin reveal the geometry of the basin and constrain models for… 
1987
1987
Synthesis of the tectonic and sedimentological evolution of the late Proterozoic-early Cambrian Hedmark Basin, the Caledonian Thrust Belt, southern Norway
The Hedmark Basin was formed by rifting c. 750-590 Ma ago in an area about 130-230 km NW of the present position of the basinal… 
Highly Cited
1986
Highly Cited
1986
THE OKINAWA TROUGH: GENESIS OF A BACK-ARC BASIN DEVELOPING ALONG A CONTINENTAL MARGIN
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