Hottentottisch. 5 : Nama, Bergdamaramundart : Homonyme ; Hottentottisch. 6 : Nama, Bergdamaramundart : einzelne Sätze / gespr. von Missionar Baumann

[Traditions. Afrique du sud. Namibie. Khoïkhoï]

Hottentottisch. 3-4 : Nama, Bergdamaramundart : einzelne Wörter / gespr. von Missionar Baumann

[Traditions. Afrique du sud. Namibie. Khoïkhoï]

Hottentottisch. Faces 1-2 : Nama, Bergdamaramundart : einzelne Wörter / gespr. von Missionar Baumann

[Traditions. Afrique du sud. Namibie. Khoïkhoï]

[Archives de la parole]. , Stances sanskrites / Hari Chand, voix

Enregistrement : Paris, Université de Paris, La Sorbonne, 04-02-1914

[Archives de la parole]. , Sur le carnage / [Haïm] Harari, chant

Enregistrement : Paris, Université de Paris, La Sorbonne, 10-03-1914

[Archives de la parole]. , [Araka taroukan] : chanson d'amour arabe / Ben Kori Alexis, chant

Enregistrement : Paris, Université de Paris, La Sorbonne, 04-02-1914

[Archives de la parole]. , Steluţa / Mlle Mioara Georgesco, chant

[Traditions. Europe. Roumanie]

[Archives de la parole]. , C'est après... je suis né dans les montagnes ; Vous aimiez bien petite mère / De Calvas, chant

[Traditions. Europe. Pologne]

[Archives de la parole]. , Belle enfant de la montagne ; Ah ! mon gas, combien nous nous aimons / Mlle Romanitsa [i. e. Romanitza], chant

[Traditions. Europe. Roumanie]

[Archives de la parole]. , Foaie verde, foi de foi / [Mademoiselle] Romanitza, chant

[Traditions. Europe. Roumanie]

[Archives de la parole]. , Biaini / M. Alexis Ben Kori, chant. Première surate du Coran / M. Alexis Ben Kori, voix

Enregistrement : Paris, Université de Paris, La Sorbonne, 28-01-1914

[Archives de la parole]. , Conversation sur l'histoire de la littérature chinoise / Sin-Pin-Chang & Tchéou-Wei, voix

Enregistrement : Paris, Université de Paris, La Sorbonne, 10-06-1913

Felher in der Stimmbildung und ihre Ursachen. 9 / nachgeahmt von Frl. Hoffmann

Enregistrement : [Hambourg], [Phonetisches Laboratorium des Seminars F. Kolon Sprachen], 00-00-1912

Influence of anatomical variations on lumbar foraminal stenosis pathogenesis.

INTRODUCTION: Symptomatic foraminal stenosis has been observed in patients with degenerative disc disease, scoliosis, asymmetrical disc degeneration and spondylolisthesis. Nevertheless not all patients with the above pathologies will develop symptomatic foraminal stenosis. We hypothesised that symptomatic patients have anatomical predisposition to foraminal stenosis, namely a larger pedicle height (PH) to vertebral body height (VH) ratio, leaving less room below the pedicle for the exiting nerve root compared to asymptomatic patients. PATIENT SAMPLE: 66 Patients were divided in two groups. The surgical group consisted of 37 patients (average age of 61 years) who presented with severe radicular symptoms resisting to conservative measures and requiring decompression and transforaminal lumbar interbody fusion (TLIF). The control group consisted of 29 patients (average age of 51 years) presenting with low back pain (LBP) but with no radicular symptoms and who were treated conservatively. METHODS: We measured VH at the level of the posterior wall as well as PH on parasagittal images (CT or MRI) on all lumbar levels (L1 to L5). Statistical analysis was performed using Student's t test. RESULTS: No difference in PH was found between the two groups for L1 to L4 levels. By contrast, there was a highly statistically significant difference in VH between the two groups from L1 to L4 level. In the surgical group, the VH was smaller (p < 0.001). CONCLUSIONS: Symptomatic patients with foraminal stenosis have smaller VH leading to lesser space beneath the pedicle and putting the exiting nerve root at risk in cases of spondylolisthesis or disc degeneration.

Formation of chlorite during thrust fault reactivation. Record of fluid origin and P-T conditions in the Monte Perdido thrust fault (southern Pyrenees)

The chemical and isotopic compositions of clay minerals such as illite and chlorite are commonly used to quantify diagenetic and low-grade metamorphic conditions, an approach that is also used in the present study of the Monte Perdido thrust fault from the South Pyrenean fold-and-thrust belt. The Monte Perdido thrust fault is a shallow thrust juxtaposing upper Cretaceous-Paleocene platform carbonates and Lower Eocene marls and turbidites from the Jaca basin. The core zone of the fault, about 6 m thick, consists of intensely deformed clay-bearing rocks bounded by major shear surfaces. Illite and chlorite are the main hydrous minerals in the fault zone. Illite is oriented along cleavage planes while chlorite formed along shear veins (< 50 mu m in thickness). Authigenic chlorite provides essential information about the origin of fluids and their temperature. delta O-18 and delta D values of newly formed chlorite support equilibration with sedimentary interstitial water, directly derived from the local hanging wall and footwall during deformation. Given the absence of large-scale fluid flow, the mineralization observed in the thrust faults records the P-T conditions of thrust activity. Temperatures of chlorite formation of about 240A degrees C are obtained via two independent methods: chlorite compositional thermometers and oxygen isotope fractionation between cogenetic chlorite and quartz. Burial depth conditions of 7 km are determined for the Monte Perdido thrust reactivation, coupling calculated temperature and fluid inclusion isochores. The present study demonstrates that both isotopic and thermodynamic methods applied to clay minerals formed in thrust fault are useful to help constrain diagenetic and low-grade metamorphic conditions.