Therapist-client similarity on the Multimodal Structural Profile

1991 ◽  
Author(s):  
Steven Herman
Keyword(s):  
Structural Profile

Wood and Bark Anatomy of Lauraceae. ii. Licaria Aublet

IAWA Journal ◽  
1985 ◽  
Vol 6 (3) ◽  
pp. 187-199 ◽  
Author(s):  
Hans Georg Richter
Keyword(s):  
Diagnostic Tool ◽  
Secondary Xylem ◽  
Secondary Phloem ◽  
Structural Profile ◽  
Quantitative Characters ◽  
Important Diagnostic Tool ◽  
Species Groups ◽  
Bark Anatomy

Qualitative features of the secondary xylem of Licaria present a rather uniform structural profile. Constant differences in primarily quantitative characters lead to the formation of speeies groups wh ich loosely correspond to infrageneric sections based on floral and vegetative morphology. This subdivision is strongly corroborated by the highly variable secondary phloem structurc revealing considerable diversity in type and distribution of sc1erenchymatic tissues. Inorganic inclusions in the secondary xylem, crystals and silica, constitute an important diagnostic tool for differentiating certain species and species groups, but are hardly of importance in the bark.

scholarly journals Biochemical, histopathological and ultra structural profile after pulsed water medication of enrofloxacin in broiler chickens

2013 ◽  
Vol 6 (9) ◽  
pp. 668-673 ◽  
Author(s):  
Veerapandian Sureshkumar ◽  
Ghadevaru Sarathchandra ◽  
Jayaramachandran Ramesh
Keyword(s):  
Broiler Chickens ◽  
Structural Profile

Structural profile of the northwestern Caribbean

1972 ◽  
Vol 17 (1) ◽  
pp. 175-180 ◽  
Author(s):  
W.P. Dillon ◽  
J.G. Vedder ◽  
R.J. Graf
Keyword(s):  
Structural Profile

1.—Dalradian Structure and Stratigraphy of the Northern Loch Awe District, Argyllshire

1973 ◽  
Vol 69 (1) ◽  
pp. 1-21 ◽  
Author(s):  
G. J. Borradaile
Keyword(s):  
Lower Cambrian ◽  
Secondary Structures ◽  
Fold Belt ◽  
Middle Cambrian ◽  
Structural Profile ◽  
Submarine Lava ◽  
Lava Sequence ◽  
Lava Pile ◽  
Stratigraphic Succession ◽  
Present Area

SynopsisA structural profile has been constructed for part of the Caledonian fold belt from a map of the Dalradian rocks of the Loch Awe District of Argyllshire. The profile includes the Loch Awe Syncline (Bailey 1913) and the root to the Tay Nappe (Shackleton 1958). The Loch Awe Syncline is shown to be a compound syncline of F1 age, congruent with the Tay Nappe. The F1 structures are accompanied by a penetrative deformation and modified by secondary structures. The stratigraphic succession, which includes the Upper Dalradian and part of the Middle Dalradian, has been reconstructed from the profiles and is shown to have originally been about 10 km thick. The prominent features are the development of a basin to the south-east of the present area in the Late Pre-Cambrian and the extrusion of a 2 km thick basic submarine lava pile in Lower Cambrian times. A subsequent basic submarine lava sequence was extruded in Late Lower Cambrian or Middle Cambrian time and represents the topmos lithostratigraphic group yet recorded from the Dalradian of S.W. Argyll.

Sign in / Sign up

Export Citation Format

Share Document