8/28/2023 0 Comments Slack 4.25.2![]() ![]() 16 He said, “At this season, in due time, you shall embrace a son.” She replied, “No, my lord, O man of God do not deceive your servant.” ( F)ġ7 The woman conceived and bore a son at that season, in due time, as Elisha had declared to her.ġ8 When the child was older, he went out one day to his father among the reapers. ( E) 13 He said to him, “Say to her: Since you have taken all this trouble for us, what may be done for you? Would you have a word spoken on your behalf to the king or to the commander of the army?” She answered, “I live among my own people.” 14 He said, “What then may be done for her?” Gehazi answered, “Well, she has no son, and her husband is old.” 15 He said, “Call her.” When he had called her, she stood at the door. 12 He said to his servant Gehazi, “Call the Shunammite woman.” When he had called her, she stood before him. ( D) 10 Let us make a small roof chamber with walls and put there for him a bed, a table, a chair, and a lamp, so that he can stay there whenever he comes to us.”ġ1 One day when he came there, he went up to the chamber and lay down there. ( C) 9 She said to her husband, “Look, I am sure that this man who regularly passes our way is a holy man of God. So whenever he passed that way, he would stop there for a meal. 7 She came and told the man of God, and he said, “Go sell the oil and pay your debts, and you and your children can live on the rest.” ( B) Elisha Raises the Shunammite’s SonĨ One day Elisha was passing through Shunem, where a wealthy woman lived, who urged him to have a meal. ![]() 6 When the vessels were full, she said to her son, “Bring me another vessel.” But he said to her, “There are no more.” Then the oil stopped flowing. 4 Then go in, shut the door behind you and your children, and start pouring into all these vessels when each is full, set it aside.” 5 So she left him and shut the door behind her and her children they kept bringing vessels to her, and she kept pouring. The Nd-Pb isotopic attributes can be used in exploration for additional REE deposits in the Mesoproterozoic rocks of the eastern Granite-Rhyolite Province.4 Now the wife of a member of the company of prophets cried to Elisha, “Your servant my husband is dead, and you know that your servant feared the Lord, but a creditor has come to take my two children as slaves.” ( A) 2 Elisha said to her, “What shall I do for you? Tell me, what do you have in the house?” She answered, “Your servant has nothing in the house except a jar of oil.” 3 He said, “Go outside, borrow vessels from all your neighbors, empty vessels-and not just a few. The Pea Ridge deposit represents an excellent example of an igneous-dominated hydrothermal system and defines a distinctive Nd-Pb isotopic target that involved coeval igneous magmatism and REE mineralization. No evidence exists for major overprinting by younger, crustal meteoric fluids, or by externally derived Nd. Pb isotope results for the felsic hosts overlap those of galena in the REE-breccia ore. Whole rock Pb isotopes of REE-rich breccia, Fe-ores and host rocks have a wide range in values and are more radiogenic than galena. The Nd and Pb isotope data indicate that the Pea Ridge deposit was part of a system that produced a uniform isotopic composition. Our results suggest that host rocks, REE-rich breccias, and Fe-ores share a common origin from a similar source. ![]() The felsic host rocks are depleted in HFSE (e.g., Nb, Ta, Ti, P) and Sr, and lack positive Pb anomalies in mantle-normalized plots. Nd isotope data show: (1) felsic hosts have e Nd values from 3.44 to 4.25 (2) REE-rich breccias have similar e Nd values from 3.04 to 4.11 (3) Fe-ores display e Nd values from 3.04 to 4.21. ![]() Immobile trace elements (e.g., Nb/Y, Zr/Ti) indicate that the felsic host rocks are subalkaline dacite and rhyolite having geochemical attributes typical of rocks produced by subduction. Nd isotope data yield depleted mantle model ages (T DM) of ~1.51 to 1.59 Ga for rhyolites, 1.51 to 1.6 Ga for REE-rich breccias, and 1.51 to 1.6 Ga for Fe-ores. Radiogenic 207Pb/ 206Pb age estimates for host rocks and ores are broadly coeval: ~1.50 Ga for rhyolitic host rocks, ~1.48 Ga for REE-rich breccias, ~1.43 Ga for Fe-ores these estimates are similar to zircon U-Pb ages determined for the host rocks and mineralizing events (ca. REE-rich breccias and iron oxide-apatite (IOA) ores at Pea Ridge are hosted in a volcanic sequence dominated by felsic tuffs with minor mafic-intermediate composition rocks. Nd and Pb isotope data were obtained on the Pea Ridge Fe-oxide-apatite-rare earth element (REE) deposit and host rocks in order to characterize their petrologic setting, better understand the regional geologic framework, and advance exploration techniques. ![]()
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