AGR与RGR的比较可进一步证明一茬草后期的管理对草群总生物量的形成具有重要的作用。
Through comparative study of AGR and RGR, it was further testified that later management of the first crop had an important effect on formation of total aboveground biomass.
重质稠油藏的形成主要受盆地后期抬升活动、生物降解、地层水洗和氧化作用等因素控制。
The formation of heavy oil reservoirs is chiefly controlled by late uplifting of the basin, biodegradation, water-washing, and free oxygen oxidizing.
原生裂缝是岩浆冷凝结晶过程中形成的裂缝；次生裂缝是火山岩及其原生裂缝系统受后期构造运动、溶蚀、风化等作用改造而形成的裂缝。
Primary fracture were formed during the lava crystal and the secondary fracture generated during the volcanic reconstruction by tectonic movement, and wind action, solution.
在试验条件下，随着施氮量的增加，氮肥对生土地大豆根瘤形成的抑制作用加大，但对大豆后期根系的生长有促进作用。
Within the condition of this study, the inhibition that the nitrogenous fertilizer takes shape to the raw soil soybean nodule increased along with the increasing of nitrogen used.
各工业矿体的形成与后期叠加构造和热流体的改造作用密切相关。
The formation of economic ore bodies is closely related to the structures superimposed later and the the...
在交代作用后期，更多的花岗岩形成，这些花岗岩可再熔化，熔化后又会凝固并被交代流体作用。
More granitic rocks are produced in the late-stage of metasomatism, which could be remelt, and each successive melt could be solidified and modified by metasomatic fluids.
同生沉积（成岩）作用形成矿源层，后期改造（叠加）形成矿体。
The metallogenetic model is that the ore origin bed was formed by syngenetic sedimentation (diagenesis) and the ore body by the later reformation (superimposition).
盆地形成后期火山作用微弱。
同时酸性流体使长石溶蚀形成高岭石，后期的风化淋滤作用使砂岩中的高岭石含量进一步提高，进而形成目前较大规模的高岭土矿床。
At the same time, acid fluid dissolved feldspar grains and transformed feldspar into kaolinite. Kaolin deposits experience later weathering and leaching and improve present scale.
中生代后期，太平洋板块的俯冲作用使胶南地体拉分，断陷形成胶莱盆地。
During the late Mesozoic, because of subduction of the Pacific plate, the Jiaonan terrain was pulled apart and experienced an event of fault depressing, hence forming the Jiaolai Basin.
现今不整合体系的形成与地质历史时期地层所受的风化、剥蚀和大气水淋滤作用及后期的水进沉积作用关系密切。
The present unconformity system is resulted from paleoweathering zone undergoing weathering, eluviations and transgression in geological age. The vertical texture existed in the both systems.
沉积作用控制了碎屑岩杂基、分选、磨圆等结构特征，进而控制了原生孔隙结构，为后期溶解作用的形成奠定了基础。
Sedimentation controlled the textures of clastic rocks such as matrix, sorting and rounding, and further affected the texture of primary pores, which served as basement for later dissolution.
最晚期的正断裂体现出来的拉张作用推测与本区推覆构造形成后期的滑脱作用有关。
The last group of faults, which is also the latest, was supposed to be related to the decollement process of the nappe structure in this area.
最晚期的正断裂体现出来的拉张作用推测与本区推覆构造形成后期的滑脱作用有关。
The last group of faults, which is also the latest, was supposed to be related to the decollement process of the nappe structure in this area.
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