جيب بركاني · الجيوب البركانية
جيب بركاني في الجيولوجيا هو تسرب الصهارة عرضيا بين طبقات من اللابة أو الأحجار الرسوبية أو الطفة البركانية أو حتى عبر شقوق في الصخور المتحولة.
岩床
(geology) a flat (usually horizontal) mass of igneous rock between two layers of older sedimentary rock
sill · Geologic sill · Geological sill · Igneous sill · Submarine sill
(geology) a flat (usually horizontal) mass of igneous rock between two layers of older sedimentary rock
More definitions
Sill · Filon-couche
Un sill ou filon-couche est une couche de roche magmatique souvent horizontale qui s'est infiltrée entre des couches plus anciennes de roche sédimentaire, de roche volcanique ou le long de la foliation d'une roche métamorphique, ce qui le différencie du filon.
Lagergang · Sill
Ein Lagergang oder Sill ist ein schichtparallel in ein Gestein eingedrungener Gesteinskörper aus magmatischem Gestein oder seltener aus sedimentärem Gestein.
στρωματοειδής φλέβα
(geology) a flat (usually horizontal) mass of igneous rock between two layers of older sedimentary rock
סיל
סיל הוא מונח בגאולוגיה לציון מחדר פלוטוני הנוצר מחדירת מאגמה לסלעי הליתוספירה והתגבשותה לסלע פלוטוני.
देहली From automatic translation
(geology) a flat (usually horizontal) mass of igneous rock between two layers of older sedimentary rock
Filone-strato · Filoni-strato · Sill · Sillis
I filoni-strato sono delle forme di intrusione magmatica, più nello specifico rientrano nelle intrusioni concordanti, termine con il quale si indica un'intrusione i cui strati sono parallel alla superficie di stratificazione delle rocce nella quale esse sono intruse., i quali sono inseriti tra uno strato e l'altro nelle rocce sedimentarie, tabulari, il cui spessore è variabile da qualche centimetro a qualche decina di metri.
силл
Силл — интрузивное тело, имеющее форму слоя, контакты которого параллельны слоистости вмещающей толщи.
Lámina (geología) · Lamina · Sill
En geología, una lámina[1] o manto [2] es una masa tabular de roca ígnea, con frecuencia horizontal, que ha intruido lateralmente entre dos capas antiguas de roca sedimentaria, capas de lava volcánica o toba volcánica, o a favor de la foliación en rocas metamórficas.
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