. Gesammelte Reprints, Essa Institut für Ozeanographie. Ozeanographie Zeitschriften.. Insel ARC SYSTEM IN der Andaman See 1809? •*';^Ich £ r,; "â¢;;;;;;;;;! •,; W;: • {â ¢. Abb. 5. âSection 4, fix 639, südwestlich-nordöstlich Profil. Sedimente im Südwesten (links) gegen harte Grundgestein oder volcanics in Richtung Nordosten zu verschwinden. Masse am Nordosten ist westlichen Block der inneren vulkanischen Bogen, angeblich ein Horst blockieren. Eine Störung wird an der rechten Seite des Bildes postuliert, upthrown in Richtung Nordosten. Für Anbauort, siehe Abbildungen 2 und 4. Verdienste eingedrungen, vielleicht so viel wie so Prozent in einigen Fällen. Unten Abt.

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. Collected reprints, Essa Institute for Oceanography. Oceanography Periodicals.. ISLAND ARC SYSTEM IN ANDAMAN SEA 1809 ?â¢*';^i£r , ;"'â¢;;; ! â¢, ; â w; :â¢{â¢. Fig. 5.âSection 4, fix 639, southwest-northeast profile. Sediments on southwest (left) are seen to disappear against hard bedrock or volcanics toward northeast. Mass on northeast is western block of inner volcanic arc, supposedly a horst block. A fault is postulated at right side of picture, upthrown toward north- east. For location, see Figures 2 and 4. merits penetrated, perhaps as much as SO per cent in some cases. Bottom depths change greatly throughout the Andaman Sea; therefore instru- mental scale shifts were frequent. The results of the sub-bottom profiler surveys are discussed from south to north. NORTHERN SUMATRAâSECTIONS 4 AND 5 The two profiles just north of Sumatra were made in order to cross known trends of major proportions. Section 4 (Fig. 4) begins on the east flank of the outer island arc, which plunges steep- ly into the interdeep. Clear evidence of sedimen- tation is lacking, possibly because of the rugged- ness and steepness of the slope. However, bed- ding and some indications of faulting can be seen at the top of the arc. Simalur Island, on the south, is a geanticline cut by north-south-trending transverse faults (Van Bemmelen, 1949). From the interdeep to fix 639 several unconformities are detectable. Sediments Southwest of fix 639 (section 4, Fig. 4) disappear against hard bed- rock or volcanics on the northeast (Fig. 5). The mass on the northeast is the western block of the inner volcanic arcâa horst. A fault is postulated at fix 639, section 4 (Fig. 4), upthrown toward the northeast. The part of section 4 from fix 639 to 648 is the offshore continuation of the pre-Tertiary and lower Tertiary block-mountain system of north- ern Sumatra. The block is represented by the western side of the Atjeh graben and the islands west of the Bengal Passage. There is a lack o

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