700 resultados para Shield-emblem


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Obverse: In the center stylized inscription. Reverse: Emblem of the Israel Government Coins and Medals Corporation.

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5 Silver coin set in olive-wood box with certificates. Obverse: 25 Silver Lirot coin. In the lower part big emblem of the State of Israel. Reverse: Five pomegranate flowers round a five-pointed star.

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3 pieces commemorative coin set in a box. 2 silver coins, 1 gold coin. Obverse: 25 Lirot silver coins, 500 Lirot gold coin. In the center the state emblem of the State of Israel. Reverse: Portrait of David Ben-Gurion.

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Peritoneal washing cytology (PWC) is a useful indicator of ovarian surface involvement and peritoneal dissemination by ovarian tumours. It may identify subclinical peritoneal spread and thus provide valuable staging and prognostic information, particularly for non-serous ovarian tumours. The role of PWC as a prognostic indicator for endometrial carcinoma is less clear, due in part to the questionable significance of identifying endometrial tumour cells in the peritoneum. Detection of metastatic carcinoma in PWC is based on recognition of non-mesothelial cell characteristics, however a number of conditions such as reactive mesothelial cells, endometriosis and endosalpingiosis may mimic this appearance. Cells from these conditions may have a similar presentation in PWC to that of serous borderline tumours and low grade serous carcinoma. The presence of cilia, lack of single atypical cells, prominent cytoplasmic vacuolation, marked nuclear atypia or two distinct cell populations are features favouring a benign process. Attention to these features along with close correlation with clinical history and the results of surgical pathology should help avoid errors. Additional assistance may be provided by the use of cell blocks and special stains.

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Aim of this study is to investigate composition of the crust in Finland using seismic wide-angle velocity models and laboratory measurements on P- and S-wave velocities of different rock types. The velocities adopted from wide-angle velocity models were compared with laboratory velocities of different rock types corrected for the crustal PT conditions in the study area. The wide-angle velocity models indicate that the P-wave velocity does not only increase step-wise at boundaries of major crustal layers, but there is also gradual increase of velocity within the layers. On the other hand, the laboratory measurements of velocities indicate that no single rock type is able to provide the gradual downward increasing trends. Thus, there must be gradual vertical changes in rock composition. The downward increase of velocities indicates that the composition of the crust becomes gradually more mafic with increasing depth. Even though single rock types cannot simulate the wide-angle model velocities, it can be done with a mixture of rock types. There are a large number of rock type mixtures giving the correct P-wave velocities. Therefore, the inverse solution of rock types and their proportions from velocities is a non-unique problem if only P-wave velocities is available. Amount of the possible rock type mixtures can be limitted using S-wave velocities, reflection seismic results and other geological and geophysical results of the study area. Crustal model FINMIX-2 is presented in this study and it suggest that the crustal velocity profiles can be simulated with rock type mixtures, where the upper crust consists of felsic gneisses and granitic-granodioritic rocks with a minor contribution of quartzite, amphibolite and diabase. In the middle crust the amphibolite proportion increases. The lower crust consists of tonalitic gneiss, mafic garnet granulite, hornblendite, pyroxenite and minor mafic eclogite. This composition model is in agreement with deep crustal kimberlite-hosted xenolith data in eastern Finland and reflectivity of the FIRE (Finnish Reflection Experiment). According to FINMIX-2 model the Moho is deeper and the crustal composition is a more mafic than an average global continental model would suggest. Composition models of southern Finland are quite similar than FINMIX-2 model. However, there are minor differencies between the models, which indicates areal differences of composition. Models of northern Finland shows that the crustal thickness is smaller than southern Finland and composition of the upper crust is different. Density profiles calculated from the lithological models suggest that there is practically no density contrast at Moho in areas of the high-velocity lower crust. This implies that crustal thickness in the central Fennoscandian Shield may have been controlled by the densities of the lower crustal and upper mantle rocks.

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Silver 10 Lirot coin. Obverse: 10 Lirot coin, emblem of the State of Israel. Reverse: Two arches and inscription.

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Silver 10 Lirot coin. Obverse: On the upper left nominal value 10 Lirot. Underneath the emblem of the State of Israel Reverse: 5 silver Shekalim minted in Jerusalem during the period of the war of the Jews against the Romans.

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Silver 10 Lirot coin. Obverse: Emblem of the State of Israel. Reverse: Two arches.

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Silver 10 Lirot coin. Obverse: Emblem of the State of Israel. Reverse: Two arches.

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Silver 5 Lirot coin. Obverse: 5 Lirot coin, emblem of State of Israel. Reverse: A Russian Hanukkah lamp

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Obverse: In the center the emblem of the Israel Defense Forces, against a stylized star. Reverse: The Western Wall.

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Silver 5 Lirot coin. Obverse: 5 Lirot, emblem of the state of Israel. Reverse: Russian Hanukkah lamp.

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Silver 10 Lirot coin. Obverse: 10 Lirot coin, emblem of the State of Israel. Reverse: 5 silver Sheqalim from Jerusalem from the period of the war of the Jews against the Romans.

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Obverse: 1 Sheqel silver coin, emblem of the State of Israel. Reverse: Hanukkah lamp from Corfu, 19th century

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Obverse: 50 Lirot silver coin, emblem of the State of Israel. Reverse: Stylized designs of mother and two children.