deriver
发表于 2025-3-25 04:33:32
Missile Defense and the Asian Cascade,lly controlled flooding event of Late Kimmeridgian age (. ammonite zone) marks the base of Sequence B. Different sedimentary facies within this sequence constitute rich hydrocarbon source-rock shales in the Feda Graben and important reservoir sandstones on the Cod Terrace. The Sequence B/C1 transiti
nascent
发表于 2025-3-25 09:50:37
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撤退
发表于 2025-3-25 12:11:42
D. Rajasekhar,R. Manjula,T. Paranjothion the northern margin of the Norwegian-Danish Basin. It is a frontier area expected to be opened for exploration within the next few years. The consequences of the uplift for the prospectivity of the Farsund Basin are illustrated, assuming the existence of a Jurassic source rock there. At its prese
归功于
发表于 2025-3-25 18:40:05
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APEX
发表于 2025-3-25 20:58:14
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Pamphlet
发表于 2025-3-26 03:41:18
,Annäherung an den Untersuchungsgegenstand, the seismic reflection attributes of siltstones or shales, are frequently cut by upper fan channellized sand-prone strata. Drilling results from the basin confirm the presence of lithofacies ranging from channellized conglomerates and sandstones to turbiditic siltstones and mudstones..The Upper Jur
Amylase
发表于 2025-3-26 06:57:37
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LEERY
发表于 2025-3-26 11:02:58
https://doi.org/10.1007/1-4020-4075-Xlts are listric and flatten out at base Tertiary level or within the Chalk. Some were already active around the end Cretaceous times, but most are Oligocene-Miocene in age, i.e. they have the same age as the dome. The radial fault pattern is characteristic of salt-induced circular domes and can be e
hauteur
发表于 2025-3-26 13:14:44
Stanley Kirschner (Professor of Chemistry) the primary organic matter production in the basin. Variations in the maturity-dependent Ts/Tm ratio and 20S/20R C29 sterane isomerization ratio occur over thicknesses of a few metres. Their correlation with the carbon isotope composition of the extracts suggests that the scatter may be related to
cutlery
发表于 2025-3-26 16:55:35
What Are Organometallic Compounds?,op..The basal Maastrichtian unit consists of thick, laterally continuous, relatively fine-grained turbidite beds, sometimes separated by thin micritic partings, with well-developed normal grading and laminations..The upper Maastrichtian-Palaeocene unit consists of very coarsegrained turbidites chara