Volatile-Oils
发表于 2025-3-23 13:43:22
Quantitative Textural Analysis of Rocks in Layered Mafic Intrusionsocess is equilibration (coarsening), testified by crystal size distributions. Almost all rocks in layered mafic intrusions have equilibrated, but the degree of progress towards equilibrium is very variable, even within layered mafic intrusions. It appears that the process is controlled by local vari
多节
发表于 2025-3-23 17:54:58
The Influence of Interfacial Energies on Igneous Microstructuresh lower structural anisotropy (e.g., olivine) form crystals with rounded to locally planar boundaries..Microstructures in partially solidified material from lava lakes and entrained glassy enclaves suggest that interfacial energies play only a minor role in the supersolidus of rapidly-cooled or coar
材料等
发表于 2025-3-23 20:43:38
Silicate Liquid Immiscibility in Layered Intrusionsformation of compositional gap along liquid lines of descent. We then present the most recent evidence for immiscibility in some major layered intrusions, i.e. the Skaergaard, Sept Iles, intrusions of the Emeishan province, and the Bushveld complex. Paired melts are identified as contrasted melt inc
chalice
发表于 2025-3-24 00:44:36
Basal Reversals in Mafic Sills and Layered Intrusionsreak. Both types of reversal are attributed to three principal processes: (1) inflowing magma becomes progressively more primitive, (2) magma undercooling gradually decreases and (3) adcumulus growth becomes increasingly more effective. The major difference between these types is that fully-develope
相反放置
发表于 2025-3-24 05:46:05
http://reply.papertrans.cn/59/5822/582137/582137_15.png
流利圆滑
发表于 2025-3-24 07:09:38
http://reply.papertrans.cn/59/5822/582137/582137_16.png
粗鲁性质
发表于 2025-3-24 10:47:44
http://reply.papertrans.cn/59/5822/582137/582137_17.png
Seizure
发表于 2025-3-24 16:35:26
http://reply.papertrans.cn/59/5822/582137/582137_18.png
CLOUT
发表于 2025-3-24 21:53:33
http://reply.papertrans.cn/59/5822/582137/582137_19.png
microscopic
发表于 2025-3-25 03:01:05
The Bushveld Complex, South Africa vertical sections to virtually absent in others. Distinctive layers (ranging from mm to many tens of m) can be identified in two or even three lobes testifying to their connectivity. Feeders to the intrusion cannot be identified, and the exact compositions (and numbers) of the parental magmas are s